kliyul - mesilinka assessment 2006 work (applied feb/07)

Kliyul - Mesilinka Assessment 2006 Work (applied Feb/07)

Property Block Date No. of Claims Event No. Work Amount UsedAssessment

Required PAC FeesKliyul Block 1 16-Feb-07 40 4133112 100,000.00 46,938.87 53,061.13 4,706.74 Kliyul Block 1a 21-Feb-07 47 4133956 60,000.00 4,580.87 55,419.13 229.67 Kliyul Block 2 15-Feb-07 62 4132905 150,000.00 70,042.37 79,957.63 6,995.06 Kliyul Block 3 16-Feb-07 51 4133031 150,000.00 56,450.65 93,549.35 5,647.80

Total 460,000.00 178,012.76 281,987.24 17,579.27

Mesilinka Block 4 16-Feb-07 60 4133170 80,000.00 73,754.26 6,245.74 7,393.53 Mesilinka Block 5 20-Feb-07 37 4133736 80,000.00 33,638.34 46,361.66 3,372.25 Mesilinka Block 6 20-Feb-07 4 4133739 8,000.00 5,011.87 2,988.13 502.56 Mesilinka Block 7 20-Feb-07 48 4133750 62,000.00 60,176.70 1,823.30 6,034.16 Mesilinka Block 8 20-Feb-07 16 4133742 9,000.00 8,507.55 492.45 853.09 Mesilinka Block 9 20-Feb-07 9 4133748 5,000.00 4,798.99 201.01 481.21 Mesilinka Block 10 26-Feb-07 8 4134630 3,000.00 2,016.31 983.69 202.05

Total 247,000.00 187,904.02 59,095.98 18,838.85

Kliyul-Mesilinka Total 707,000.00 365,916.78 341,083.22 36,418.12

Claims:Yul 9-12, Kli 51-70, Mes 1-9, Moc 1-20, Joh 1-10, Ten 1-144, Nell 1-74, Kli 1-28, 39-50, UTA 4, 6, 8, Yul 7, 8, Mes 10 Abe 7-11, Pal 1-5, Aten 1-7, Mate 1,2, Mat, Tut 1,2, Ringo, Starr, KC, PGE, Westend, Eastside, Bingo, 1 more Bango, 2 more Bingo,

i

2006 Assessment Report

Mesilinka Project

Claims: Yul 9-12, Kli 51-70, Mes 1-9, Moc 1-20, Joh 1-10, Ten 1-144, Nell 1-74, Kli 1-28, 39-50, UTA 4, 6, 8, Yul 7, 8, Abe 7-11, Pal 1-5, Aten 1-7, Mate 1,2, Mat, Tut 1,2, Ringo, Starr, KC, PGE,

Westend, Eastside, Bingo, 1 more Bango, 2 more Bingo, Mes 10

Report on Data Compilation, and Exploration for Copper-Gold Porphyry and Skarn Deposits

Omineca Mining Division

NTS 94D03-05, 94D08-10, 94D15-16

Claim Owners: Geoinformatics Exploration Canada Ltd, Commander Resources Ltd, Norwest Enterprises, Kennecott Canada Exploration Inc.

Claim Operators: Geoinformatics Exploration Canada Ltd.

Report By

John Mair

Gerry Bidwell

May 2007

Geoinformatics Exploration Canada Ltd.

Suite 304, 700 West Pender Street

Vancouver, British Columbia, Canda

V6C 1G8

ii

Executive Summary

The Mesilinka Project is a regional project in central to northern British Columbia that

comprises numerous Cu-Au alkalic porphyry and skarn deposit targets. The project

encompasses a total of 359 claims with an area of 126,664 hectares. The project area is

predominantly underlain by Mesozoic island arc assemblages of Quesnel Terrane with a

small area at the northern end of the project area underlain by similar arc assemblages of

Stikine Terrane. The project is located between the Kemess porphyry Cu-Au deposits to

the north (Kemess North – 407 Mt @ 0.22% Cu, 0.4 g/t Au), and the Lorraine porphyry

Cu-Au deposit (31.9 Mt @ 0.66% Cu, 0.17g/t Au, 4.7 g/t Ag) to the south.

The majority of claims are owned by Geoinformatics Exploration Canada Ltd, with a

number of optioned claims owned by Commander Resources Ltd and Norwest Enterprises.

In 2006, a significant database was generated through the digital capture of geochemical,

geological and geophysical datasets. This aided in constraining target areas within the large

project area. Field programs included a stream sediment sample program in which 226

samples were collected that identified several catchments with strongly anomalous Cu and

Au values. These anomalous regions will be followed up in 2007. In addition, a two hole

diamond drill program was undertaken on the Kliyul Cu-Au skarn prospect. The program

produced the most significant intercept from the project to date, with an intercept of 217.8

m @ 0.23% Cu and 0.52 g/t Au.

iii

Table of Contents

Executive Summary .............................................................................................................. ii

Table of Contents ................................................................................................................. iii

List of Figures ....................................................................................................................... v

List of Tables......................................................................................................................... v

1 Introduction ................................................................................................................... 1

1.1 Preamble................................................................................................................ 1

1.2 Project History....................................................................................................... 1

1.3 Tenure.................................................................................................................... 6

1.4 Location and Access.............................................................................................. 7

1.5 Topography and Vegetation .................................................................................. 8

1.6 Historical Work ..................................................................................................... 8

2 Regional Geology.......................................................................................................... 9

2.1 Metamorphism .................................................................................................... 11

2.2 Mineral Deposit Styles ........................................................................................ 11

3 2006 Work................................................................................................................... 13

3.1 Data Compilation ................................................................................................ 13

3.2 Field Work........................................................................................................... 14

3.3 Diamond Drilling ................................................................................................ 20

iv

4 Conclusions ................................................................................................................. 24

5 References ................................................................................................................... 25

6 Statement of Qualifications ......................................................................................... 26

Appendix 1: Claim Listing. ................................................................................................. 28

Appendix 2: Stream sediment sample location sites and assay certificates ........................ 29

Appendix 3: Kliyul diamond drill core logs, drill section and assay certificates................ 30

Appendix 4: Statement of costs (Expenditures and Assessment Data)............................... 31

v

List of Figures

Figure 1. The location of Geoinformatics’ British Columbia Cu-Au project areas within

Quesnellia, B.C... .................................................................................................................. 6

Figure 2. The location of Geoinformatics Mesilinka project area with respect to towns in

central British Columbia.. ..................................................................................................... 7

Figure 3. Simplified geology of the Mesilinka project area................................................ 10

Figure 4. Stream sediment sample locations for samples compiled from ARIS assessment

reports.................................................................................................................................. 15

Figure 5. Soil sample locations for samples compiled from ARIS assessment reports. ..... 16

Figure 6. Rock sample locations for samples compiled from ARIS assessment reports. ... 17

Figure 7. Geoinformatics 2006 stream sediment survey conducted over the southern

Mesilinka claim block. Points are plotted by copper concentration. ................................. 18

Figure 8. Geoinformatics 2006 stream sediment survey, with sample points plotted by gold

concentration. ...................................................................................................................... 19

Figure 10. Kliyul drill hole traces and the three-dimensional inversion model of ground

magnetic data that was used as a basis for drill hole targeting............................................ 23

Figure 11. Section view of three-dimensional inversion model of ground magnetic data.. 23

List of Tables

Table 1. Summary of the best intercepts from the Kliyul 2006 diamond drill program.. ... 21

1

1 Introduction

1.1 Preamble

This report describes the work completed by Geoinformatics Exploration Canada Ltd

(Geoinformatics) in 2006 on the Mesilinka project. The project is focused on exploration

for Cu- and Au-rich porphyry type deposits within central to northern Quesnel Terrane,

British Columbia (Fig. 1). The field work followed an extensive phase of digital data

capture, integration and interpretation, and subsequent regional target generation. The

majority of the field work undertaken was reconnaissance in nature, and aimed to identify

prospects within the broad project area, to be followed up on in 2007. Reconnaissance

work was focused toward areas of interest that were identified from the datasets compiled

from public domain data. A 226 stream sediment sample program was conducted over the

southern portion of the project area, where compiled stream sediment data was deemed

insufficient. In addition, a two hole diamond drill campaign totaling 751.5m on the

previously-drilled Kliyul Cu-Au skarn aimed to further evaluate its economic potential.

1.2 Project History

In 2006, Geoinformatics staked a significant land holding in northern Quesnellia and

eastern Stikinia, between the Lorraine Cu-Au deposit in the south and the Kemess Cu-Au

deposit in the north (Fig. 1). The area was staked following regional targeting exercises

that identified the region as being highly prospective for intrusion-related Cu-Au porphyry

and skarn mineralization. The staked claims form two blocks; a large southern block

extending from Tenakihi Creek to Johanson Lake, and a smaller block to the north in

McConnell Range area. Collectively the project area is referred to as the Mesilinka Project,

after the Mesilinka River which transects the southern claim block. The area includes the

Kliyul Cu-Au prospect located at the headwaters of Kliyul Creek. Numerous other Cu-Au

prospects occur in the region with most located on small claim blocks held by other

parties. The claim holding was subsequently increased through option agreements with

6

Commander Resources Ltd and Norwest Enterprises that consolidated Geoinformatics’

project area in the region.

1.3 Tenure

In total Geoinformatics’ Mesilinka Project encompasses 359 claims that cover 126,664.29

hectares. Of that total, 10 claims are owned by Norwest Enterprises (optioned by

Geoinformatics), 25 claims are owned by Commander Resources Ltd (optioned by

Geoinformatics), 47 claims are owned by Kennecott (quit-claimed to Geoinformatics), and

the remaining 276 claims are owned by Geoinformatics. The details of claim status,

ownership, tenure number, and ownership are listed in Appendix 1.

Figure 1. The location of Geoinformatics’ British Columbia Cu-Au project areas with Quesnellia. The

Mesilinka project area consists of the two northern claim blocks (see inset).

7

1.4 Location and Access

The Mesilinka project area extends over parts of NTS sheets 094D15, 094D16, 094D10,

094D09, 094D08, 094C03 - 05. The southern claim block straddles the northeastern

margin of the Hogem Batholith, within Quesnel Terrane. The northern block occurs on the

western side of the Pinchi Fault in eastern-most Stikine Terrane, and is mostly underlain by

Takla Group volcanic rocks, and felsic to intermediate intrusions of the Black Lake suite.

Together the claim blocks occupy a highly prospective corridor between the Kemess Cu-

Au deposits in the north and the Lorraine Cu-Au deposit to the south.

Figure 2. The location of Geoinformatics Mesilinka project area with respect to towns in central

British Columbia. The project area is best accessed via the Omineca Resource Access Road.

The southern end of the Mesilinka Project area is located approximately 150 km NW of

Mackenzie, B.C. (Fig. 2). Direct access to the two claim blocks is restricted by the rugged

terrain; however the general area can be accessed from the Omineca Resource Access

Omineca Resource

Access Road

8

Road from Fort St James. A network of logging roads then extend from the Omineca

Resource Access Road up the valleys into the Mesilinka project area. Airstrips are present

at Johanson Lake, located between the two claim blocks, and at the Osilinka logging camp

located to the east of the southern claim block.

1.5 Topography and Vegetation

The geomorphology of the Mesilinka project is characterized by rugged peaks and ridges

of the Omineca Mountains. The highest peaks in the region extend to elevations of up to

2400m asl, whereas major valleys in the area are at approximately 1000m asl.

Vegetation varies from forested valley bottoms of white spruce and pine to alpine

vegetation above tree line. Scrub alpine fur and willow are locally dense near the

timberline.

1.6 Historical Work

The Mesilinka Project area has been subject to a number of preliminary exploration

campaigns of regional scale, with only minor detailed work on specific prospects; the most

notable being the Kliyul Cu-Au prospect.

In the later 1960’s and early 1970’s Union Miniere Exploration and Mining Corp. Ltd

(UMEX) of Montreal conducted extensive regional exploration in the north-central British

Columbia, over part of the Mesilinka Project area. Work was carried out by Dolmage

Campbell & Associates Ltd. Detailed regional silt surveying was completed followed by

select airborne magnetic surveying and follow-up prospecting, mapping, soil sampling

along with ground magnetic and induced polarization surveying.

In 2000, Phelps Dodge Corporation conducted preliminary soil, bedrock and silt sampling

and geological mapping in the Tenakihi Creek region, which is located near the southern

end of the Mesilinka Project area. Of 83 grab samples, 23 returned greater than 0.5% Cu,

with 8 samples containing greater than 2% Cu (Kula, 2001). Monzonite to monzodiorite

intrusions were documented in the area, along with propylitc and minor potassic alteration.

9

The area surrounding the headwaters of Kliyul Creek has received multiple exploration

campaigns that commenced in the early 1970’s. Prior work includes soil and rock chip

sampling, electromagnetic and induced polarization surveys, ground and aeromagnetic

surveys, detailed geological mapping, six reverse circulation drill holes and twenty three

diamond drill holes. The majority of these drill holes were targeted on a magnetic high

that is approximately 350 x 450m. The magnetic high represents a Cu-Au bearing

magnetite-rich skarn. Drill holes did not exceed vertical depths of 120m, with the majority

of holes drilled to vertical depths of <100 m. A detailed summary of prior work on the

Kliyul prospect is summarized in Gill (1994).

A series of Cu-Au porphyry prospects are located on claims optioned from Commander

Resources. These include the Abe, Pal, Mate, Tut and Aten prospects. Considerable past

work has taken place on the Abe prospect, including ground magnetics and induced

polarization, extensive soil and rock chip sampling, and ten diamond drill holes, and is

summarized by Kalhert (2005).

2 Regional Geology

The Mesilinka Project area is situated within Quesnel Terrane, an accreted Mesozoic island

arc that forms a linear belt approximately 1600 km long. The terrane is dominated by

equivalent volcano-sedimentary sequences of the Upper Triassic to Lower Jurassic Takla,

Nicola, and Stuhini groups. Co-eval intrusions are scattered throughout. Post-accretionary

felsic intrusions of Cretaceous age are also hosted within Quesnellia. Numerous Cu-Au

porphyry deposits and abundant prospects and occurrences have been documented through

the entire belt, and are associated with high-level intrusions of Late Triassic to Early

Jurassic age. Isolated molybdenum deposits are mostly associated with Cretaceous

intrusions.

10

Figure 3. Simplified geology of the Mesilinka project area. Simplified from the BCGS 1:250,000 scale

geological map (UTM NAD 83, Zone 9).

Nelson and Bellefontaine (1996) suggest the tabular form of several intrusions in central

Quesnellia indicate arc-parallel structures that were active during emplacement.

Geoinformatics also interpreted deep-level, belt-parallel structures from the geophysics.

Also recognised were relatively evenly spaced (20-30km spaced) deep-level north-east

trending cross-arc structures (Worth and Bidwell, 2006). These appear to post-date the

belt-parallel structures but may have also been active during the island arc formation of the

Quesnel terrane. Within this regional framework, numerous smaller faults of north-west,

11

north-east and west-north-west orientation occur within the project area. Less frequent

north-trending faults also occur. Any folding present within the project area is thought to

be gentle, with dips on bedding measurements generally less than 30 degrees except when

close to intrusive margins or faults.

The Mesilinka Project area is dominantly underlain by intermediate volcanic and

volcaniclastic rocks of the Takla Group, and intrusions of the polyphase Hogem Batholith

and Abraham Creek Complex (Fig. 3). The Hogem Batholith comprises dominantly

intermediate to felsic rocks of alkalic affinity, with a younger granitic core of Cretaceous

age. The Abraham Creek Complex is an elongate body that includes mafic cumulate

phases, in addition to more evolved monzonitic and dioritic phases. Recent work by B.C.

Department of Mines geologist Paul Schiarrizara compares the Abraham Creek Complex

closely to the Iron Mask Batholith at Kamloops which hosts the large Afton copper-gold

deposits. The Kliyul Creek region, where a small drill program was carried out in 2006, is

underlain by a succession of variably calcareous volcaniclastic siltstones, and intrusive

phases associated with the Abraham Creek complex.

2.1 Metamorphism

Rocks within the project area have generally undergone metamorphism to prehnite-

pumpellyite grade and locally, adjacent to the Hogem batholith, greenschist facies (Nelson

and Bellefontaine, 1996).

2.2 Mineral Deposit Styles

The Mesilinka project area is prospective for a number of deposit styles including alkalic

porphyry copper-gold, gold and base metal skarn mineralisation, and structurally hosted

epithermal gold mineralisation.

The principle style being targeted by Geoinformatics is alkalic porphyry copper-gold

mineralisation. This style of mineralisation represents a very attractive target with

potentially large tonnages and moderate gold and copper grades, such as occurs at Galore

Creek (517.7Mt @ 0.59% Cu, 0.36g/t Au, 4.54g/t Ag). Other deposits of this type that

12

occur within central Quesnellia include Mt Milligan (445Mt @ 0.215% Cu, 0.415g/t Au),

Chuchi Lake (50Mt @ 0.21% Cu, 0.21g/t Au) and Lorraine (31.9Mt @ 0.66% Cu, 0.17g/t

Au, 4.7g/t Ag) (MINFILE database, 2005).

Skarn mineralisation is often associated with porphyry deposits where limestones exist

adjacent to the intrusions. A variably calcareous sequence of siltstones occur in the Kliyul

Creek region, and are demonstrated to host skarn-type Cu-Au mineralization.

13

3 2006 Work

3.1 Data Compilation

During 2006, an extensive phase of data capture was undertaken to compile geological and

geochemical databases for the broader Mesilinka project area. This comprised a thorough

process of data capture and conversion to digital form for incorporation into the GIS

environment. Data sets were subsequently integrated and interpreted, and utilized in

Geoinformatics refined targeting process known as MOCA. The MOCA targeting process

is a model driven method of targeting for mineral deposits using Monte Carlo probabilistic

algorithms to generate porphyry Cu-Au targets (Worth and Bidwell, 2006). Open file data

that was utilized includes published maps and technical reports, available regional

geochemical datasets, and data obtained from ARIS reports available on the British

Columbia geological survey website

(http://www.em.gov.bc.ca/Mining/Geolsurv/Aris/default.htm). Figures 4, 5 and 6 illustrate

the distribution of compiled geochemical data for stream, soil and rock samples.

An extensive database was established that consists of:

• 3168 stream sediment samples,

• 4491 rock samples

• 1455 soil samples

• 10 geophysical datasets including ground and aeromagnetic data, induced polarization surveys, electromagnetic surveys, and radiometric surveys

• mineral occurrence data from the BCGS Minfile database

• 40 drill holes, including both reverse circulation and diamond drilling

• over 30 geological outcrop maps

14

3.2 Field Work

In 2006 Geoinformatics Exploration ran an extensive field program over its Redton Project

located further south of the Mesilinka Project area. The Redton field camp served as a base

from which the majority of reconnaissance field work on Mesilinka was carried out. In

addition, as small outpost camp was established at the headwaters of Kliyul Creek that

consisted of three wall tents. This camp was supported by the larger Redton field camp,

and served as a base for the small diamond drill campaign at Kliyul.

Stream Sediment Geochemical Survey

A stream sediment survey was undertaken to aid in delineating areas of interest within the

large project area. The survey area, outlined in Figure 7 and 8, formed a corridor along the

contact between the Hogem Batholith and Takla Group volcanic rocks (Fig. 3). This region

overlaps the southern portion of the Abraham Creek complex. No stream sediment

sampling was carried out on the northern McConnell Range block, as this area featured

greater coverage of legacy data from previous campaigns by other explorers.

The survey was conducted over particularly rugged terrane and required full helicopter

support, resulting in slow progress and overall high costs per sample. A total of 226

samples were collected on Geoinformatics ground, and were analysed for 37 elements by

ICP-MS at Acme Laboritories in Vancouver, B.C. Copies of the assay certificates and

sample locations (UTM NAD83 Zone 10) are presented in Appendix 2.

The survey did return numerous samples with highly anomalous Cu concentrations that

constrain catchment areas of interest. Most notably, a series of catchments located toward

the southeast end of the Mesilinka Project area returned a number of samples with highly

elevated Cu and Au concentrations that will be an obvious area for follow up in 2007

(Figures 7 and 8). Of the samples collected, 13.3% contained >200 ppm Cu, and 3% of

samples contained > 300 ppm Cu.

15

Figure 4. Stream sediment sample locations for samples compiled from ARIS assessment reports.

Quesnellia is outlined by the light green line, whereas Stikinia is outlined by the darker green line.

Coordinates are UTM NAD83 (Zone 9).

16

Figure 5. Soil sample locations for samples compiled from ARIS assessment reports (UTM NAD83,

Zone 9).

17

Figure 6. Rock sample locations for samples compiled from ARIS assessment reports (UTM NAD83,

Zone 9).

18

Figure 7. Geoinformatics 2006 stream sediment survey conducted over the southern Mesilinka claim

block. Points are plotted by copper concentration (UTM NAD 83, Zone 9).

19

Figure 8. Geoinformatics 2006 stream sediment survey, with sample points plotted by gold

concentration (UTM NAD 83, Zone 9).

20

3.3 Diamond Drilling

In 2006 two diamond holes totaling 751.5m were drilled into the Kliyul Cu-Au magnetite

skarn, which had previously been explored with approximately 25 diamond and RC drill

holes (Fig. 9). Previous holes had mostly been drilled to vertical depths of less than 100m.

In addition, there were notable differences in the grade and continuity of intercepts from

the reverse circulation and diamond drilling. The 2006 drilling aimed to evaluate the

continuation of mineralization below that encountered in previous drilling, and in addition,

aimed to evaluate the grade and continuity of mineralization, given the discrepancies from

previous drill campaigns. Both drill holes were completed by Full Force Drilling Ltd, of

Peachland British Columbia, using a helicopter portable Mandrill 1200 hydraulic machine.

Both holes were drilled to NQ2 core size and the core orientated using an ACE Core

Orientation Tool™ to allow for collection of accurate structural measurements. Down hole

dip and azimuth surveys were collected at nominal 60 m (200ft) intervals down hole using

a Reflex Ez shot® drill hole survey tool.

All drill core was transported back to the Redton field camp located further south, for

logging and sampling. The core was cut in half using a core saw for sampling, with most

samples generally comprising 2m lengths, unless very strongly mineralized, in which one

case 1m samples were taken. All samples were collected and submitted to ACME

Analytical Laboratories Ltd., Vancouver for analysis. Samples were analyzed for a suite of

53 elements by ICPOES and ICPMS methods using a 30 gram charge. Field standards and

blanks were inserted by Geoinformatics at a ratio of 1:18 to ensure the accuracy and

reliability of results.

Drill holes were targeted on a three dimensional inversion model of a preexisting ground

magnetic survey (Figs. 10 and 11). The two holes were drilled toward the southwest

targeting a large lobe in the inversion model that represents a magnetic high. Hole

KL_06_30 was drilled to a depth of 325.37m (down hole) and hole KL_06_31 was drilled

to a depth of 751.48m. Both holes encountered strong Cu-Au mineralization, with drill

hole KL_06_30 producing the best intercept from the Kliyul project to date of 217.8 m @

0.23% Cu and 0.52 g/t Au. The best intercepts are summarized in Table 1. The drilling

21

successfully demonstrated the continuation of mineralization at depths below that tested by

previous campaigns. Drill hole logs, a drill section, and assay certificates are presented in

Appendix 3.

Table 1. Summary of the best intercepts from the Kliyul 2006 diamond drill core program. Intervals

were calculated using a 0.05% copper cut-off, with minimum width of 4 metres and maximum internal dilution of

8 metres.

Hole_Id From (m) To Interval (m) %Cu Au (ppm) Ag (ppm) Mo (ppm) KL06_30 22 239.8 217.8 0.23 0.52 1.82 5.26 KL06_30 251 259 8.0 0.05 0.21 0.54 5.04 KL06_30 275 325.37 50.4 0.10 0.28 0.60 2.47 KL06_31 20 24 4.0 0.12 0.15 2.02 14.48 KL06_31 108 194 86.0 0.13 0.26 1.09 3.91 KL06_31 230 336 106.0 0.13 0.21 1.27 3.59 KL06_31 346 376 30.0 0.23 0.61 1.11 2.68 KL06_31 392 420 28.0 0.13 0.95 1.02 1.37

22

Figure 9. Kliyul drill hole plan on the magnetite rich Cu-Au skarn prospect. The drill holes are superimposed on an

aeromagnetic RTP image. The inset in the top right of the image is a close up on the magnetic high.

23

Figure 10. Kliyul drill hole traces and the three-dimensional inversion model of ground magnetic data

that was used as a basis for drill hole targeting. Drill hole traces are colored by Cu concentration.

Figure 11. Section view of three-dimensional inversion model of ground magnetic data and drill hole

traces. The broad strongly mineralized intercept in hole KL_06_30 strongly correlates with the

modeled magnetic high body, and represents the best Cu and Au intercept from the project to date.

24

4 Conclusions

The 2006 work on Mesilinka created a database to aid in targeting for Cu-Au intrusion-

related mineral deposit types that facilitated the generation of targets within the large

project area. The data compiled included 3168 stream sediment, 4491 rock (and rock chip),

and 1455 soil samples. The regional stream sediment sample program identified a number

of strongly anomalous catchments to focus the 2007 field program and validate Cu-Au

targets identified through the data compilation process. This both confirmed the

significance of known Cu-Au prospects and Minfile occurrences, and identified new target

areas.

Two diamond drill holes were completed on the Kliyul Cu-Au skarn prospect. The holes

were targeted on three-dimensional magnetic highs generated from an inversion model of a

preexisting ground magnetic survey. The holes aimed to test the grade and continuity of

Cu-Au mineralization, as well as test the continuation of mineralization at depth. The holes

successfully demonstrated the continuation of Cu-Au mineralization at depths below that

tested by previous drill campaigns. Hole KL_06_30 returned the most significant Cu-Au

intersection from the Kliyul project to date, with an intercept of 217.8m @ 0.23% Cu and

0.52 g/t Au. These holes demonstrated that the potential resource size at Kliyul to be

significantly larger than indicated by the previous drill campaigns.

25

5 References

Gill, D.G., 1994. B.C. Drilling assessment report on the Kliyul group of claims. B.C.

Ministry of Energy, Mines and Petroleum Resources Assessment Report 23797.

Kelhert, B., 2005. Assessment Report, ABE Property, prospecting and sampling 2005.

B.C. Ministry of Energy, Mines and Petroleum Resources Assessment Report

27972.

Kulla, G., 2001. Geological and geochemical report on the Tenakihi property. Ministry of

Energy, Mines and Petroleum Resources Assessment Report 26530.

MINFILE Database, 2005. Ministry of Energy, Mines and Petroleum Resources:

http://www.em.gov.bc.ca/Mining/Geolsurv/Minfile/search/default.htm

Nelson, J.L. and Bellefontaine, K.A., 1996. The Geology and Mineral Deposits of North-

Central Quesnellia; Tezzeron Lake to Discovery Creek, Central British Columbia.

B.C. Ministry of Employment and Investment, Energy and Minerals Division,

Geological Survey Branch. Bulletin 99, 112 pages.

Worth, A. and Bidwell, G., 2006. 2005 Assessment Report, Redton property. B.C.

Ministry of Energy, Mines and Petroleum Resources Assessment Report 28264.

26

6 Statement of Qualifications

I, Gerald E. Bidwell, P.Geo., of 5186-44th Avenue, Delta, BC V4K 1C3, do hereby certify

the following:

I am a consulting geologist with G. Bidwell & Associates Ltd. of Delta, BC.

I have been practicing my profession continuously since graduation in 1967, as a geologist

in Canada and the United States of America. I worked continuously from graduation to

1996 as a geoscientist for Hudson Bay Exploration and Development Company Limited

(1967-87), Mingold Resources Inc. (1987-1990) and Noranda Exploration/Hemlo Gold

Mines (1990-96). Since 1997 I have been a principal of G. Bidwell & Associates Ltd.

I am a graduate of the University of Saskatchewan, with a Bachelor of Arts and Science

degree in Geology in 1967.

I am a Professional Geoscientist in good standing with the Association of Professional

Engineers and Geoscientists of British Columbia and a fellow of the Geological

Association of Canada.

I have been the Exploration Manager – North America for Geoinformatics Exploration Inc.

since May, 2004.

I spent 10 days on the Mesilinka property in July-August 2006.

Respectfully submitted,

Gerald E. Bidwell, P. Geo.

Dated May 14 , 2007 in Vancouver, B.C.

27

John L. Mair, BSc (Honours), PhD.

I, John Mair, PhD., of 45 Keane Street, Peppermint Grove, Perth, WA, Australia, do

hereby certify the following:

- I am a geologist employed by Geoinformatics Exploration Australia Ltd.

- I have been practicing my profession from 1998 – 2000, and from 2004 to present (PhD research 2000 – 2004) as a geologist in Australia, Alaska, China and Canada.

- I am a graduate of the University of Western Australia, with a Bachelor of Science, Honours degree (geology), 1997, and PhD (geology)

- I was the project manager for the Mesilinka and Kliyul projects in 2006.

Dated May 14 , 2007 in Vancouver, B.C.

28

Appendix 1: Claim Listing.

Omineca Mining District, British Columbia

Claim Owner Issue Tenure NTS Map Area ExpiryName Date No. Number (hectares) 07 08 09 10 11

MOC1 Geoinformatics Exploration Canada Limited 06-Jun-06 534992 094D 392.932 February 28, 2008 X 1,571.73 1,571.73 3,143.46 3,143.46 MOC2 Geoinformatics Exploration Canada Limited 06-Jun-06 534993 094D 428.839 February 28, 2008 X 1,715.36 1,715.36 3,430.71 3,430.71 MOC3 Geoinformatics Exploration Canada Limited 06-Jun-06 534994 094D 411.136 February 28, 2008 X 1,644.54 1,644.54 3,289.09 3,289.09 MOC4 Geoinformatics Exploration Canada Limited 06-Jun-06 534995 094D 446.687 February 28, 2008 X 1,786.75 1,786.75 3,573.50 3,573.50 MOC5 Geoinformatics Exploration Canada Limited 06-Jun-06 534996 094D 446.726 February 28, 2008 X 1,786.90 1,786.90 3,573.81 3,573.81

Geoinformatics Exploration Canada Limited 06-Jun-06 534997 094D 429.056 February 28, 2008 X 1,716.22 1,716.22 3,432.45 3,432.45 MOC7 Geoinformatics Exploration Canada Limited 06-Jun-06 534998 094D 429.221 February 28, 2008 X 1,716.88 1,716.88 3,433.77 3,433.77 MOC8 Geoinformatics Exploration Canada Limited 06-Jun-06 534999 094D 429.032 February 28, 2008 X 1,716.13 1,716.13 3,432.26 3,432.26 MOC9 Geoinformatics Exploration Canada Limited 06-Jun-06 535000 094D 357.836 February 28, 2008 X 1,431.34 1,431.34 2,862.69 2,862.69 MOC10 Geoinformatics Exploration Canada Limited 06-Jun-06 535001 094D 250.609 February 28, 2008 X 1,002.44 1,002.44 2,004.87 2,004.87 MOC11 Geoinformatics Exploration Canada Limited 06-Jun-06 535002 094D 429.855 February 28, 2008 X 1,719.42 1,719.42 3,438.84 3,438.84 MOC12 Geoinformatics Exploration Canada Limited 06-Jun-06 535003 094D 447.143 February 28, 2008 X 1,788.57 1,788.57 3,577.14 3,577.14 MOC13 Geoinformatics Exploration Canada Limited 06-Jun-06 535004 094D 429.161 February 28, 2008 X 1,716.64 1,716.64 3,433.29 3,433.29 MOC14 Geoinformatics Exploration Canada Limited 06-Jun-06 535005 094D 447.219 February 28, 2008 X 1,788.88 1,788.88 3,577.75 3,577.75 MOC15 Geoinformatics Exploration Canada Limited 06-Jun-06 535006 094D 447.413 February 28, 2008 X 1,789.65 1,789.65 3,579.30 3,579.30 MOC16 Geoinformatics Exploration Canada Limited 06-Jun-06 535007 094D 375.976 February 28, 2008 X 1,503.90 1,503.90 3,007.81 3,007.81 MOC17 Geoinformatics Exploration Canada Limited 06-Jun-06 535008 094C 447.817 February 28, 2008 X 1,791.27 1,791.27 3,582.54 3,582.54 MOC18 Geoinformatics Exploration Canada Limited 06-Jun-06 535009 094D 447.823 February 28, 2008 X 1,791.29 1,791.29 3,582.58 3,582.58 MOC19 Geoinformatics Exploration Canada Limited 06-Jun-06 535010 094D 447.831 February 28, 2008 X 1,791.32 1,791.32 3,582.65 3,582.65 MOC20 Geoinformatics Exploration Canada Limited 06-Jun-06 535011 094D 447.877 February 28, 2008 X 1,791.51 1,791.51 3,583.02 3,583.02 JOH1 Geoinformatics Exploration Canada Limited 06-Jun-06 535012 094D 446.3 February 28, 2008 X 1,785.20 1,785.20 3,570.40 3,570.40 JOH2 Geoinformatics Exploration Canada Limited 06-Jun-06 535013 094D 446.283 February 28, 2008 X 1,785.13 1,785.13 3,570.26 3,570.26 JOH3 Geoinformatics Exploration Canada Limited 06-Jun-06 535014 094D 446.058 February 28, 2008 X 1,784.23 1,784.23 3,568.46 3,568.46 JOH4 Geoinformatics Exploration Canada Limited 06-Jun-06 535015 094D 428.209 February 28, 2008 X 1,712.84 1,712.84 3,425.67 3,425.67 JOH5 Geoinformatics Exploration Canada Limited 06-Jun-06 535016 094D 446.03 February 28, 2008 X 1,784.12 1,784.12 3,568.24 3,568.24 JOH006 Geoinformatics Exploration Canada Limited 06-Jun-06 535017 094D 427.932 February 28, 2008 X 1,711.73 1,711.73 3,423.46 3,423.46 JOH8 Geoinformatics Exploration Canada Limited 06-Jun-06 535018 094D 428.002 February 28, 2008 X 1,712.01 1,712.01 3,424.02 3,424.02 JOH8 Geoinformatics Exploration Canada Limited 06-Jun-06 535019 094D 445.456 February 28, 2008 X 1,781.82 1,781.82 3,563.65 3,563.65 JOH9 Geoinformatics Exploration Canada Limited 06-Jun-06 535020 094D 445.647 February 28, 2008 X 1,782.59 1,782.59 3,565.18 3,565.18 JOH10 Geoinformatics Exploration Canada Limited 07-Jun-06 535021 094D 445.522 February 28, 2008 X 1,782.09 1,782.09 3,564.18 3,564.18 TEN1 Geoinformatics Exploration Canada Limited 07-Jun-06 535023 094C 451.047 February 28, 2008 X 1,804.19 1,804.19 3,608.38 3,608.38 TEN2 Geoinformatics Exploration Canada Limited 07-Jun-06 535024 094C 450.822 February 28, 2008 X 1,803.29 1,803.29 3,606.58 3,606.58 TEN3 Geoinformatics Exploration Canada Limited 07-Jun-06 535025 094C 432.539 February 28, 2008 X 1,730.16 1,730.16 3,460.31 3,460.31 TEN4 Geoinformatics Exploration Canada Limited 07-Jun-06 535026 094C 72.123 February 28, 2008 X 288.49 288.49 576.98 576.98 TEN5 Geoinformatics Exploration Canada Limited 07-Jun-06 535027 094C 450.724 February 28, 2008 X 1,802.90 1,802.90 3,605.79 3,605.79 TEN6 Geoinformatics Exploration Canada Limited 07-Jun-06 535028 094C 432.368 February 28, 2008 X 1,729.47 1,729.47 3,458.94 3,458.94 TEN7 Geoinformatics Exploration Canada Limited 07-Jun-06 535029 094C 432.509 February 28, 2008 X 1,730.04 1,730.04 3,460.07 3,460.07 TEN8 Geoinformatics Exploration Canada Limited 07-Jun-06 535031 094C 450.583 February 28, 2008 X 1,802.33 1,802.33 3,604.66 3,604.66 TEN9 Geoinformatics Exploration Canada Limited 07-Jun-06 535033 094C 450.822 February 28, 2008 X 1,803.29 1,803.29 3,606.58 3,606.58 TEN10 Geoinformatics Exploration Canada Limited 07-Jun-06 535034 094C 450.611 February 28, 2008 X 1,802.44 1,802.44 3,604.89 3,604.89 TEN11 Geoinformatics Exploration Canada Limited 07-Jun-06 535037 094C 450.611 February 28, 2008 X 1,802.44 1,802.44 3,604.89 3,604.89 TEN12 Geoinformatics Exploration Canada Limited 07-Jun-06 535040 094C 414.55 February 28, 2008 X 1,658.20 1,658.20 3,316.40 3,316.40 TEN13 Geoinformatics Exploration Canada Limited 07-Jun-06 535041 094C 450.367 February 28, 2008 X 1,801.47 1,801.47 3,602.94 3,602.94 TEN14 Geoinformatics Exploration Canada Limited 07-Jun-06 535042 094C 450.124 February 28, 2008 X 1,800.50 1,800.50 3,600.99 3,600.99 TEN15 Geoinformatics Exploration Canada Limited 07-Jun-06 535043 094C 450.117 February 28, 2008 X 1,800.47 1,800.47 3,600.94 3,600.94

Yearly Assessment Requirements

Mesilinka Project Claim ListingGeoinformatics Exploration Canada Limited

1 of 6 11/05/2007





TEN16 Geoinformatics Exploration Canada Limited 07-Jun-06 535044 094C 450.121 February 28, 2008 X 1,800.48 1,800.48 3,600.97 3,600.97 TEN17 Geoinformatics Exploration Canada Limited 07-Jun-06 535045 094C 395.893 February 28, 2008 X 1,583.57 1,583.57 3,167.14 3,167.14 TEN18 Geoinformatics Exploration Canada Limited 07-Jun-06 535046 094C 449.629 February 28, 2008 X 1,798.52 1,798.52 3,597.03 3,597.03 TEN19 Geoinformatics Exploration Canada Limited 07-Jun-06 535047 094C 449.634 February 28, 2008 X 1,798.54 1,798.54 3,597.07 3,597.07 TEN20 Geoinformatics Exploration Canada Limited 07-Jun-06 535048 094C 449.631 February 28, 2008 X 1,798.52 1,798.52 3,597.05 3,597.05 TEN22 Geoinformatics Exploration Canada Limited 07-Jun-06 535049 094C 449.717 February 28, 2008 X 1,798.87 1,798.87 3,597.74 3,597.74 TEN21 Geoinformatics Exploration Canada Limited 07-Jun-06 535051 094C 450.356 February 28, 2008 X 1,801.42 1,801.42 3,602.85 3,602.85 TEN23 Geoinformatics Exploration Canada Limited 07-Jun-06 535052 094C 450.359 February 28, 2008 X 1,801.44 1,801.44 3,602.87 3,602.87 TEN24 Geoinformatics Exploration Canada Limited 07-Jun-06 535053 094C 432.513 February 28, 2008 X 1,730.05 1,730.05 3,460.10 3,460.10 TEN25 Geoinformatics Exploration Canada Limited 07-Jun-06 535054 094C 432.384 February 28, 2008 X 1,729.54 1,729.54 3,459.07 3,459.07 TEN26 Geoinformatics Exploration Canada Limited 07-Jun-06 535055 094C 450.836 February 28, 2008 X 1,803.34 1,803.34 3,606.69 3,606.69 TEN27 Geoinformatics Exploration Canada Limited 07-Jun-06 535056 094C 450.964 February 28, 2008 X 1,803.86 1,803.86 3,607.71 3,607.71 TEN28 Geoinformatics Exploration Canada Limited 07-Jun-06 535057 094C 451.203 February 28, 2008 X 1,804.81 1,804.81 3,609.62 3,609.62 TEN29 Geoinformatics Exploration Canada Limited 07-Jun-06 535058 094C 433.312 February 28, 2008 X 1,733.25 1,733.25 3,466.50 3,466.50 TEN30 Geoinformatics Exploration Canada Limited 07-Jun-06 535059 094C 451.062 February 28, 2008 X 1,804.25 1,804.25 3,608.50 3,608.50 TEN31 Geoinformatics Exploration Canada Limited 07-Jun-06 535060 094C 433.203 February 28, 2008 X 1,732.81 1,732.81 3,465.62 3,465.62 TEN32 Geoinformatics Exploration Canada Limited 07-Jun-06 535061 094C 451.069 February 28, 2008 X 1,804.28 1,804.28 3,608.55 3,608.55 TEN33 Geoinformatics Exploration Canada Limited 07-Jun-06 535062 094C 433.314 February 28, 2008 X 1,733.26 1,733.26 3,466.51 3,466.51 TEN34 Geoinformatics Exploration Canada Limited 07-Jun-06 535063 094C 415.202 February 28, 2008 X 1,660.81 1,660.81 3,321.62 3,321.62 TEN 35 Geoinformatics Exploration Canada Limited 07-Jun-06 535064 094C 450.841 February 28, 2008 X 1,803.36 1,803.36 3,606.73 3,606.73 TEN36 Geoinformatics Exploration Canada Limited 07-Jun-06 535068 094C 451.086 February 28, 2008 X 1,804.34 1,804.34 3,608.69 3,608.69 TEN37 Geoinformatics Exploration Canada Limited 07-Jun-06 535071 094C 433.047 February 28, 2008 X 1,732.19 1,732.19 3,464.38 3,464.38 TEN38 Geoinformatics Exploration Canada Limited 07-Jun-06 535074 094C 450.831 February 28, 2008 X 1,803.32 1,803.32 3,606.65 3,606.65 TEN39 Geoinformatics Exploration Canada Limited 07-Jun-06 535075 094C 451.062 February 28, 2008 X 1,804.25 1,804.25 3,608.50 3,608.50 TEN40 Geoinformatics Exploration Canada Limited 07-Jun-06 535077 094C 449.877 February 28, 2008 X 1,799.51 1,799.51 3,599.02 3,599.02 TEN41 Geoinformatics Exploration Canada Limited 07-Jun-06 535081 094C 449.592 February 28, 2008 X 1,798.37 1,798.37 3,596.74 3,596.74 TEN42 Geoinformatics Exploration Canada Limited 07-Jun-06 535087 094C 431.376 February 28, 2008 X 1,725.50 1,725.50 3,451.01 3,451.01 TEN43 Geoinformatics Exploration Canada Limited 07-Jun-06 535121 094C 431.39 February 28, 2008 X 1,725.56 1,725.56 3,451.12 3,451.12 TEN44 Geoinformatics Exploration Canada Limited 07-Jun-06 535122 094C 431.134 February 28, 2008 X 1,724.54 1,724.54 3,449.07 3,449.07 TEN45 Geoinformatics Exploration Canada Limited 07-Jun-06 535123 094C 395.214 February 28, 2008 X 1,580.86 1,580.86 3,161.71 3,161.71 TEN46 Geoinformatics Exploration Canada Limited 07-Jun-06 535124 094C 449.372 February 28, 2008 X 1,797.49 1,797.49 3,594.98 3,594.98 TEN47 Geoinformatics Exploration Canada Limited 07-Jun-06 535125 094C 449.334 February 28, 2008 X 1,797.34 1,797.34 3,594.67 3,594.67 TEN48 Geoinformatics Exploration Canada Limited 07-Jun-06 535127 094C 431.197 February 28, 2008 X 1,724.79 1,724.79 3,449.58 3,449.58 TEN49 Geoinformatics Exploration Canada Limited 07-Jun-06 535128 094C 413.151 February 28, 2008 X 1,652.60 1,652.60 3,305.21 3,305.21 TEN50 Geoinformatics Exploration Canada Limited 07-Jun-06 535129 094C 448.998 February 28, 2008 X 1,795.99 1,795.99 3,591.98 3,591.98 TEN52 Geoinformatics Exploration Canada Limited 07-Jun-06 535130 094C 448.747 1,794.99 1,794.99 3,589.98 3,589.98 TEN51 Geoinformatics Exploration Canada Limited 07-Jun-06 535131 094C 430.605 February 28, 2008 X 1,722.42 1,722.42 3,444.84 3,444.84 TEN53 Geoinformatics Exploration Canada Limited 07-Jun-06 535132 094C 430.67 February 28, 2008 X 1,722.68 1,722.68 3,445.36 3,445.36 TEN54 Geoinformatics Exploration Canada Limited 07-Jun-06 535133 094C 448.808 February 28, 2008 X 1,795.23 1,795.23 3,590.46 3,590.46 TEN55 Geoinformatics Exploration Canada Limited 07-Jun-06 535134 094C 448.889 February 28, 2008 X 1,795.56 1,795.56 3,591.11 3,591.11 TEN56 Geoinformatics Exploration Canada Limited 07-Jun-06 535135 094C 447.974 February 28, 2008 X 1,791.90 1,791.90 3,583.79 3,583.79 TEN57 Geoinformatics Exploration Canada Limited 07-Jun-06 535136 094C 447.839 February 28, 2008 X 1,791.36 1,791.36 3,582.71 3,582.71 TEN58 Geoinformatics Exploration Canada Limited 07-Jun-06 535137 094C 448.034 February 28, 2008 X 1,792.14 1,792.14 3,584.27 3,584.27 TEN59 Geoinformatics Exploration Canada Limited 07-Jun-06 535142 094C 304.547 February 28, 2008 X 1,218.19 1,218.19 2,436.38 2,436.38 TEN60 Geoinformatics Exploration Canada Limited 07-Jun-06 535144 094C 448.651 February 28, 2008 X 1,794.60 1,794.60 3,589.21 3,589.21

2 of 6 11/05/2007





TEN61 Geoinformatics Exploration Canada Limited 07-Jun-06 535145 094C 430.338 February 28, 2008 X 1,721.35 1,721.35 3,442.70 3,442.70 TEN62 Geoinformatics Exploration Canada Limited 07-Jun-06 535147 094C 448.43 February 28, 2008 X 1,793.72 1,793.72 3,587.44 3,587.44 TEN64 Geoinformatics Exploration Canada Limited 07-Jun-06 535148 094C 448.74 February 28, 2008 X 1,794.96 1,794.96 3,589.92 3,589.92 TEN63 Geoinformatics Exploration Canada Limited 07-Jun-06 535149 094C 448.728 February 28, 2008 X 1,794.91 1,794.91 3,589.82 3,589.82 TEN65 Geoinformatics Exploration Canada Limited 07-Jun-06 535150 094C 448.88 February 28, 2008 X 1,795.52 1,795.52 3,591.04 3,591.04 TEN66 Geoinformatics Exploration Canada Limited 07-Jun-06 535151 094C 450.012 February 28, 2008 X 1,800.05 1,800.05 3,600.10 3,600.10 TEN67 Geoinformatics Exploration Canada Limited 07-Jun-06 535152 094C 432.219 February 28, 2008 X 1,728.88 1,728.88 3,457.75 3,457.75 TEN68 Geoinformatics Exploration Canada Limited 07-Jun-06 535153 094C 288.145 February 28, 2008 X 1,152.58 1,152.58 2,305.16 2,305.16 TEN69 Geoinformatics Exploration Canada Limited 07-Jun-06 535154 094C 432.667 February 28, 2008 X 1,730.67 1,730.67 3,461.34 3,461.34 TEN70 Geoinformatics Exploration Canada Limited 07-Jun-06 535155 094C 450.877 February 28, 2008 X 1,803.51 1,803.51 3,607.02 3,607.02 TEN71 Geoinformatics Exploration Canada Limited 07-Jun-06 535156 094C 451.084 February 28, 2008 X 1,804.34 1,804.34 3,608.67 3,608.67 TEN72 Geoinformatics Exploration Canada Limited 07-Jun-06 535157 094C 451.397 February 28, 2008 X 1,805.59 1,805.59 3,611.18 3,611.18 TEN73 Geoinformatics Exploration Canada Limited 07-Jun-06 535158 094C 451.087 February 28, 2008 X 1,804.35 1,804.35 3,608.70 3,608.70 TEN74 Geoinformatics Exploration Canada Limited 07-Jun-06 535159 094C 451.123 February 28, 2008 X 1,804.49 1,804.49 3,608.98 3,608.98 TEN75 Geoinformatics Exploration Canada Limited 07-Jun-06 535160 094C 451.261 February 28, 2008 X 1,805.04 1,805.04 3,610.09 3,610.09 TEN76 Geoinformatics Exploration Canada Limited 07-Jun-06 535161 094C 450.858 February 28, 2008 X 1,803.43 1,803.43 3,606.86 3,606.86 TEN77 Geoinformatics Exploration Canada Limited 07-Jun-06 535162 094C 432.576 February 28, 2008 X 1,730.30 1,730.30 3,460.61 3,460.61 TEN78 Geoinformatics Exploration Canada Limited 07-Jun-06 535163 094C 450.875 February 28, 2008 X 1,803.50 1,803.50 3,607.00 3,607.00 TEN79 Geoinformatics Exploration Canada Limited 07-Jun-06 535164 094C 432.622 February 28, 2008 X 1,730.49 1,730.49 3,460.98 3,460.98 TEN80 Geoinformatics Exploration Canada Limited 07-Jun-06 535165 094C 449.959 February 28, 2008 X 1,799.84 1,799.84 3,599.67 3,599.67 TEN81 Geoinformatics Exploration Canada Limited 07-Jun-06 535167 094C 450.188 February 28, 2008 X 1,800.75 1,800.75 3,601.50 3,601.50 TEN82 Geoinformatics Exploration Canada Limited 07-Jun-06 535168 094C 450.2 February 28, 2008 X 1,800.80 1,800.80 3,601.60 3,601.60 TEN83 Geoinformatics Exploration Canada Limited 07-Jun-06 535169 094C 450.452 February 28, 2008 X 1,801.81 1,801.81 3,603.62 3,603.62 TEN84 Geoinformatics Exploration Canada Limited 07-Jun-06 535170 094C 450.432 February 28, 2008 X 1,801.73 1,801.73 3,603.46 3,603.46 TEN85 Geoinformatics Exploration Canada Limited 07-Jun-06 535171 094C 450.408 February 28, 2008 X 1,801.63 1,801.63 3,603.26 3,603.26 TEN86 Geoinformatics Exploration Canada Limited 07-Jun-06 535172 094C 450.575 February 28, 2008 X 1,802.30 1,802.30 3,604.60 3,604.60 TEN87 Geoinformatics Exploration Canada Limited 07-Jun-06 535173 094C 450.614 February 28, 2008 X 1,802.46 1,802.46 3,604.91 3,604.91 TEN88 Geoinformatics Exploration Canada Limited 07-Jun-06 535174 094C 450.337 February 28, 2008 X 1,801.35 1,801.35 3,602.70 3,602.70 TEN89 Geoinformatics Exploration Canada Limited 07-Jun-06 535175 094C 450.364 February 28, 2008 X 1,801.46 1,801.46 3,602.91 3,602.91 TEN90 Geoinformatics Exploration Canada Limited 07-Jun-06 535176 094C 450.086 February 28, 2008 X 1,800.34 1,800.34 3,600.69 3,600.69 TEN91 Geoinformatics Exploration Canada Limited 07-Jun-06 535177 094C 449.864 February 28, 2008 X 1,799.46 1,799.46 3,598.91 3,598.91 TEN92 Geoinformatics Exploration Canada Limited 07-Jun-06 535178 094C 432.149 February 28, 2008 X 1,728.60 1,728.60 3,457.19 3,457.19 TEN93 Geoinformatics Exploration Canada Limited 07-Jun-06 535180 094C 449.622 February 28, 2008 X 1,798.49 1,798.49 3,596.98 3,596.98 TEN94 Geoinformatics Exploration Canada Limited 07-Jun-06 535181 094C 431.94 February 28, 2008 X 1,727.76 1,727.76 3,455.52 3,455.52 TEN95 Geoinformatics Exploration Canada Limited 07-Jun-06 535183 094C 431.926 February 28, 2008 X 1,727.70 1,727.70 3,455.41 3,455.41 TEN96 Geoinformatics Exploration Canada Limited 07-Jun-06 535184 094C 449.684 February 28, 2008 X 1,798.74 1,798.74 3,597.47 3,597.47 TEN97 Geoinformatics Exploration Canada Limited 07-Jun-06 535185 094C 449.411 February 28, 2008 X 1,797.64 1,797.64 3,595.29 3,595.29 TEN98 Geoinformatics Exploration Canada Limited 07-Jun-06 535186 094C 431.156 February 28, 2008 X 1,724.62 1,724.62 3,449.25 3,449.25 TEN99 Geoinformatics Exploration Canada Limited 07-Jun-06 535187 094C 448.632 February 28, 2008 X 1,794.53 1,794.53 3,589.06 3,589.06 TEN100 Geoinformatics Exploration Canada Limited 07-Jun-06 535188 094C 430.957 February 28, 2008 X 1,723.83 1,723.83 3,447.66 3,447.66 TEN101 Geoinformatics Exploration Canada Limited 07-Jun-06 535189 094C 430.952 February 28, 2008 X 1,723.81 1,723.81 3,447.62 3,447.62 TEN102 Geoinformatics Exploration Canada Limited 07-Jun-06 535191 094C 449.191 February 28, 2008 X 1,796.76 1,796.76 3,593.53 3,593.53 TEN103 Geoinformatics Exploration Canada Limited 07-Jun-06 535192 094C 449.253 February 28, 2008 X 1,797.01 1,797.01 3,594.02 3,594.02 TEN104 Geoinformatics Exploration Canada Limited 07-Jun-06 535193 094C 287.784 February 28, 2008 X 1,151.14 1,151.14 2,302.27 2,302.27 TEN105 Geoinformatics Exploration Canada Limited 07-Jun-06 535194 094C 287.669 February 28, 2008 X 1,150.68 1,150.68 2,301.35 2,301.35

3 of 6 11/05/2007





TEN106 Geoinformatics Exploration Canada Limited 07-Jun-06 535195 094C 447.515 February 28, 2008 X 1,790.06 1,790.06 3,580.12 3,580.12 TEN107 Geoinformatics Exploration Canada Limited 07-Jun-06 535196 094C 447.763 February 28, 2008 X 1,791.05 1,791.05 3,582.10 3,582.10 TEN108 Geoinformatics Exploration Canada Limited 08-Jun-06 535200 094C 447.51 February 28, 2008 X 1,790.04 1,790.04 3,580.08 3,580.08 TEN109 Geoinformatics Exploration Canada Limited 08-Jun-06 535201 094C 447.708 February 28, 2008 X 1,790.83 1,790.83 3,581.66 3,581.66 TEN110 Geoinformatics Exploration Canada Limited 08-Jun-06 535202 094C 447.763 February 28, 2008 X 1,791.05 1,791.05 3,582.10 3,582.10 TEN111 Geoinformatics Exploration Canada Limited 08-Jun-06 535203 094C 447.998 February 28, 2008 X 1,791.99 1,791.99 3,583.98 3,583.98 TEN112 Geoinformatics Exploration Canada Limited 08-Jun-06 535205 094C 430.314 February 28, 2008 X 1,721.26 1,721.26 3,442.51 3,442.51 TEN113 Geoinformatics Exploration Canada Limited 08-Jun-06 535206 094C 447.956 February 28, 2008 X 1,791.82 1,791.82 3,583.65 3,583.65 TEN114 Geoinformatics Exploration Canada Limited 08-Jun-06 535207 094C 447.977 February 28, 2008 X 1,791.91 1,791.91 3,583.82 3,583.82 TEN115 Geoinformatics Exploration Canada Limited 08-Jun-06 535208 094C 448.203 February 28, 2008 X 1,792.81 1,792.81 3,585.62 3,585.62 TEN116 Geoinformatics Exploration Canada Limited 08-Jun-06 535209 094C 430.222 February 28, 2008 X 1,720.89 1,720.89 3,441.78 3,441.78 TEN117 Geoinformatics Exploration Canada Limited 08-Jun-06 535210 094C 448.316 February 28, 2008 X 1,793.26 1,793.26 3,586.53 3,586.53 TEN118 Geoinformatics Exploration Canada Limited 08-Jun-06 535212 094C 448.624 February 28, 2008 X 1,794.50 1,794.50 3,588.99 3,588.99 TEN119 Geoinformatics Exploration Canada Limited 08-Jun-06 535214 094C 448.645 February 28, 2008 X 1,794.58 1,794.58 3,589.16 3,589.16 TEN120 Geoinformatics Exploration Canada Limited 08-Jun-06 535216 094C 448.651 February 28, 2008 X 1,794.60 1,794.60 3,589.21 3,589.21 TEN121 Geoinformatics Exploration Canada Limited 08-Jun-06 535219 094C 448.46 February 28, 2008 X 1,793.84 1,793.84 3,587.68 3,587.68 TEN122 Geoinformatics Exploration Canada Limited 08-Jun-06 535221 094C 448.877 February 28, 2008 X 1,795.51 1,795.51 3,591.02 3,591.02 TEN123 Geoinformatics Exploration Canada Limited 08-Jun-06 535222 094C 449.128 February 28, 2008 X 1,796.51 1,796.51 3,593.02 3,593.02 TEN124 Geoinformatics Exploration Canada Limited 08-Jun-06 535225 094C 449.4 February 28, 2008 X 1,797.60 1,797.60 3,595.20 3,595.20 TEN125 Geoinformatics Exploration Canada Limited 08-Jun-06 535228 094C 449.689 February 28, 2008 X 1,798.76 1,798.76 3,597.51 3,597.51 TEN126 Geoinformatics Exploration Canada Limited 08-Jun-06 535234 094C 449.949 February 28, 2008 X 1,799.80 1,799.80 3,599.59 3,599.59 TEN127 Geoinformatics Exploration Canada Limited 08-Jun-06 535235 094C 450.208 February 28, 2008 X 1,800.83 1,800.83 3,601.66 3,601.66 TEN128 Geoinformatics Exploration Canada Limited 08-Jun-06 535237 094C 450.466 February 28, 2008 X 1,801.86 1,801.86 3,603.73 3,603.73 TEN129 Geoinformatics Exploration Canada Limited 08-Jun-06 535239 094C 448.917 February 28, 2008 X 1,795.67 1,795.67 3,591.34 3,591.34 TEN131 Geoinformatics Exploration Canada Limited 08-Jun-06 535242 094C 449.163 February 28, 2008 X 1,796.65 1,796.65 3,593.30 3,593.30 TEN130 Geoinformatics Exploration Canada Limited 08-Jun-06 535243 094C 449.446 February 28, 2008 X 1,797.78 1,797.78 3,595.57 3,595.57 TEN132 Geoinformatics Exploration Canada Limited 08-Jun-06 535245 094C 449.724 February 28, 2008 X 1,798.90 1,798.90 3,597.79 3,597.79 TEN133 Geoinformatics Exploration Canada Limited 08-Jun-06 535246 094C 449.979 February 28, 2008 X 1,799.92 1,799.92 3,599.83 3,599.83 TEN134 Geoinformatics Exploration Canada Limited 08-Jun-06 535248 094C 450.233 February 28, 2008 X 1,800.93 1,800.93 3,601.86 3,601.86 TEN135 Geoinformatics Exploration Canada Limited 08-Jun-06 535249 094C 450.484 February 28, 2008 X 1,801.94 1,801.94 3,603.87 3,603.87 TEN136 Geoinformatics Exploration Canada Limited 08-Jun-06 535251 094C 450.666 February 28, 2008 X 1,802.66 1,802.66 3,605.33 3,605.33 TEN137 Geoinformatics Exploration Canada Limited 08-Jun-06 535254 094C 448.87 February 28, 2008 X 1,795.48 1,795.48 3,590.96 3,590.96 TEN138 Geoinformatics Exploration Canada Limited 08-Jun-06 535256 094C 449.115 February 28, 2008 X 1,796.46 1,796.46 3,592.92 3,592.92 TEN139 Geoinformatics Exploration Canada Limited 08-Jun-06 535258 094C 449.387 February 28, 2008 X 1,797.55 1,797.55 3,595.10 3,595.10 TEN140 Geoinformatics Exploration Canada Limited 08-Jun-06 535261 094C 449.678 February 28, 2008 X 1,798.71 1,798.71 3,597.42 3,597.42 TEN141 Geoinformatics Exploration Canada Limited 08-Jun-06 535263 094C 449.933 February 28, 2008 X 1,799.73 1,799.73 3,599.46 3,599.46 TEN142 Geoinformatics Exploration Canada Limited 08-Jun-06 535265 094C 450.186 February 28, 2008 X 1,800.74 1,800.74 3,601.49 3,601.49 TEN143 Geoinformatics Exploration Canada Limited 08-Jun-06 535267 094C 360.327 February 28, 2008 X 1,441.31 1,441.31 2,882.62 2,882.62 TEN144 Geoinformatics Exploration Canada Limited 08-Jun-06 535268 094C 360.474 February 28, 2008 X 1,441.90 1,441.90 2,883.79 2,883.79 NELL1 Geoinformatics Exploration Canada Limited 08-Jun-06 535276 094D 441.988 February 28, 2008 X 1,767.95 1,767.95 3,535.90 3,535.90 NELL2 Geoinformatics Exploration Canada Limited 08-Jun-06 535278 094D 441.991 February 28, 2008 X 1,767.96 1,767.96 3,535.93 3,535.93 NELL3 Geoinformatics Exploration Canada Limited 08-Jun-06 535280 094D 441.999 February 28, 2008 X 1,768.00 1,768.00 3,535.99 3,535.99 NELL4 Geoinformatics Exploration Canada Limited 08-Jun-06 535282 094D 442.231 February 28, 2008 X 1,768.92 1,768.92 3,537.85 3,537.85 NELL5 Geoinformatics Exploration Canada Limited 08-Jun-06 535283 094D 442.235 February 28, 2008 X 1,768.94 1,768.94 3,537.88 3,537.88 NELL6 Geoinformatics Exploration Canada Limited 08-Jun-06 535285 094D 442.243 February 28, 2008 X 1,768.97 1,768.97 3,537.94 3,537.94

4 of 6 11/05/2007





NELL7 Geoinformatics Exploration Canada Limited 08-Jun-06 535286 094D 442.49 February 28, 2008 X 1,769.96 1,769.96 3,539.92 3,539.92 NELL8 Geoinformatics Exploration Canada Limited 08-Jun-06 535287 094D 442.481 February 28, 2008 X 1,769.92 1,769.92 3,539.85 3,539.85 NELL9 Geoinformatics Exploration Canada Limited 08-Jun-06 535288 094D 442.477 February 28, 2008 X 1,769.91 1,769.91 3,539.82 3,539.82 NELL10 Geoinformatics Exploration Canada Limited 08-Jun-06 535289 094D 442.459 February 28, 2008 X 1,769.84 1,769.84 3,539.67 3,539.67 NELL11 Geoinformatics Exploration Canada Limited 08-Jun-06 535290 094D 407.069 February 28, 2008 X 1,628.28 1,628.28 3,256.55 3,256.55 NELL12 Geoinformatics Exploration Canada Limited 08-Jun-06 535292 094D 442.698 February 28, 2008 X 1,770.79 1,770.79 3,541.58 3,541.58 NELL13 Geoinformatics Exploration Canada Limited 08-Jun-06 535293 094D 442.705 February 28, 2008 X 1,770.82 1,770.82 3,541.64 3,541.64 NELL14 Geoinformatics Exploration Canada Limited 08-Jun-06 535294 094D 442.726 February 28, 2008 X 1,770.90 1,770.90 3,541.81 3,541.81 NELL15 Geoinformatics Exploration Canada Limited 08-Jun-06 535295 094D 442.731 February 28, 2008 X 1,770.92 1,770.92 3,541.85 3,541.85 NELL17 Geoinformatics Exploration Canada Limited 08-Jun-06 535296 094D 442.74 February 28, 2008 X 1,770.96 1,770.96 3,541.92 3,541.92 NELL16 Geoinformatics Exploration Canada Limited 08-Jun-06 535297 094D 442.986 February 28, 2008 X 1,771.94 1,771.94 3,543.89 3,543.89 NELL18 Geoinformatics Exploration Canada Limited 08-Jun-06 535298 094D 442.978 February 28, 2008 X 1,771.91 1,771.91 3,543.82 3,543.82 NELL19 Geoinformatics Exploration Canada Limited 08-Jun-06 535299 094D 442.973 February 28, 2008 X 1,771.89 1,771.89 3,543.78 3,543.78 NELL20 Geoinformatics Exploration Canada Limited 08-Jun-06 535300 094D 442.953 February 28, 2008 X 1,771.81 1,771.81 3,543.62 3,543.62 NELL21 Geoinformatics Exploration Canada Limited 08-Jun-06 535302 094D 442.945 February 28, 2008 X 1,771.78 1,771.78 3,543.56 3,543.56 NELL22 Geoinformatics Exploration Canada Limited 08-Jun-06 535303 094D 443.193 February 28, 2008 X 1,772.77 1,772.77 3,545.54 3,545.54 NELL23 Geoinformatics Exploration Canada Limited 08-Jun-06 535304 094D 443.2 February 28, 2008 X 1,772.80 1,772.80 3,545.60 3,545.60 NELL24 Geoinformatics Exploration Canada Limited 08-Jun-06 535305 094D 443.219 February 28, 2008 X 1,772.88 1,772.88 3,545.75 3,545.75 NELL25 Geoinformatics Exploration Canada Limited 08-Jun-06 535306 094D 443.224 February 28, 2008 X 1,772.90 1,772.90 3,545.79 3,545.79 NELL26 Geoinformatics Exploration Canada Limited 08-Jun-06 535307 094D 443.253 February 28, 2008 X 1,773.01 1,773.01 3,546.02 3,546.02 NELL27 Geoinformatics Exploration Canada Limited 08-Jun-06 535314 094D 443.485 February 28, 2008 X 1,773.94 1,773.94 3,547.88 3,547.88 NELL28 Geoinformatics Exploration Canada Limited 08-Jun-06 535315 094D 443.478 February 28, 2008 X 1,773.91 1,773.91 3,547.82 3,547.82 NELL29 Geoinformatics Exploration Canada Limited 08-Jun-06 535316 094D 443.458 February 28, 2008 X 1,773.83 1,773.83 3,547.66 3,547.66 NELL30 Geoinformatics Exploration Canada Limited 08-Jun-06 535317 094D 443.449 February 28, 2008 X 1,773.80 1,773.80 3,547.59 3,547.59 NELL31 Geoinformatics Exploration Canada Limited 08-Jun-06 535318 094D 443.924 February 28, 2008 X 1,775.70 1,775.70 3,551.39 3,551.39 NELL33 Geoinformatics Exploration Canada Limited 08-Jun-06 535319 094D 443.719 February 28, 2008 X 1,774.88 1,774.88 3,549.75 3,549.75 NELL32 Geoinformatics Exploration Canada Limited 08-Jun-06 535320 094D 443.725 February 28, 2008 X 1,774.90 1,774.90 3,549.80 3,549.80 NELL34 Geoinformatics Exploration Canada Limited 08-Jun-06 535321 094D 443.71 February 28, 2008 X 1,774.84 1,774.84 3,549.68 3,549.68 NELL35 Geoinformatics Exploration Canada Limited 08-Jun-06 535322 094D 443.696 February 28, 2008 X 1,774.78 1,774.78 3,549.57 3,549.57 NELL36 Geoinformatics Exploration Canada Limited 08-Jun-06 535323 094D 443.678 February 28, 2008 X 1,774.71 1,774.71 3,549.42 3,549.42 NELL37 Geoinformatics Exploration Canada Limited 08-Jun-06 535324 094D 426.187 February 28, 2008 X 1,704.75 1,704.75 3,409.50 3,409.50 NELL38 Geoinformatics Exploration Canada Limited 08-Jun-06 535325 094D 443.953 February 28, 2008 X 1,775.81 1,775.81 3,551.62 3,551.62 NELL39 Geoinformatics Exploration Canada Limited 08-Jun-06 535326 094D 443.938 February 28, 2008 X 1,775.75 1,775.75 3,551.50 3,551.50 NELL40 Geoinformatics Exploration Canada Limited 08-Jun-06 535327 094D 426.132 February 28, 2008 X 1,704.53 1,704.53 3,409.06 3,409.06 NELL41 Geoinformatics Exploration Canada Limited 08-Jun-06 535328 094D 426.189 February 28, 2008 X 1,704.76 1,704.76 3,409.51 3,409.51 NELL42 Geoinformatics Exploration Canada Limited 08-Jun-06 535329 094D 444.21 February 28, 2008 X 1,776.84 1,776.84 3,553.68 3,553.68 NELL43 Geoinformatics Exploration Canada Limited 08-Jun-06 535330 094D 444.196 February 28, 2008 X 1,776.78 1,776.78 3,553.57 3,553.57 NELL44 Geoinformatics Exploration Canada Limited 08-Jun-06 535332 094D 444.193 February 28, 2008 X 1,776.77 1,776.77 3,553.54 3,553.54 NELL45 Geoinformatics Exploration Canada Limited 08-Jun-06 535333 094D 444.178 February 28, 2008 X 1,776.71 1,776.71 3,553.42 3,553.42 NELL46 Geoinformatics Exploration Canada Limited 08-Jun-06 535334 094D 444.384 February 28, 2008 X 1,777.54 1,777.54 3,555.07 3,555.07 NELL47 Geoinformatics Exploration Canada Limited 08-Jun-06 535335 094D 284.404 February 28, 2008 X 1,137.62 1,137.62 2,275.23 2,275.23 NELL48 Geoinformatics Exploration Canada Limited 08-Jun-06 535336 094D 195.528 February 28, 2008 X 782.11 782.11 1,564.22 1,564.22 NELL49 Geoinformatics Exploration Canada Limited 24-Oct-06 543939 094D 171.910 February 28, 2008 X 687.64 687.64 1,375.28 1,375.28 NELL50 Geoinformatics Exploration Canada Limited 24-Oct-06 543959 094D 172.050 February 28, 2008 X 688.20 688.20 1,376.40 1,376.40 NELL51 Geoinformatics Exploration Canada Limited 24-Oct-06 543979 094D 172.050 February 28, 2008 X 688.20 688.20 1,376.40 1,376.40

5 of 6 11/05/2007





NELL52 Geoinformatics Exploration Canada Limited 24-Oct-06 543999 094D 172.040 February 28, 2008 X 688.16 688.16 1,376.32 1,376.32 NELL53 Geoinformatics Exploration Canada Limited 24-Oct-06 544019 094D 171.990 February 28, 2008 X 687.96 687.96 1,375.92 1,375.92 NELL54 Geoinformatics Exploration Canada Limited 24-Oct-06 544039 094D 164.770 February 28, 2008 X 659.08 659.08 1,318.16 1,318.16 NELL55 Geoinformatics Exploration Canada Limited 24-Oct-06 544059 094D 179.110 February 28, 2008 X 716.44 716.44 1,432.88 1,432.88 NELL56 Geoinformatics Exploration Canada Limited 24-Oct-06 544061 094D 179.110 February 28, 2008 X 716.44 716.44 1,432.88 1,432.88 NELL57 Geoinformatics Exploration Canada Limited 24-Oct-06 544079 094D 172.610 February 28, 2008 X 690.44 690.44 1,380.88 1,380.88 NELL58 Geoinformatics Exploration Canada Limited 24-Oct-06 544099 094D 172.690 February 28, 2008 X 690.76 690.76 1,381.52 1,381.52 NELL59 Geoinformatics Exploration Canada Limited 24-Oct-06 544119 094D 172.750 February 28, 2008 X 691.00 691.00 1,382.00 1,382.00 NELL60 Geoinformatics Exploration Canada Limited 24-Oct-06 544139 094D 179.870 February 28, 2008 X 719.48 719.48 1,438.96 1,438.96 NELL61 Geoinformatics Exploration Canada Limited 24-Oct-06 544159 094D 179.930 February 28, 2008 X 719.72 719.72 1,439.44 1,439.44 NELL62 Geoinformatics Exploration Canada Limited 24-Oct-06 544199 094D 179.770 February 28, 2008 X 719.08 719.08 1,438.16 1,438.16 NELL63 Geoinformatics Exploration Canada Limited 24-Oct-06 544179 094D 151.090 February 28, 2008 X 604.36 604.36 1,208.72 1,208.72 NELL64 Geoinformatics Exploration Canada Limited 24-Oct-06 544219 094D 172.610 February 28, 2008 X 690.44 690.44 1,380.88 1,380.88 NELL65 Geoinformatics Exploration Canada Limited 24-Oct-06 544239 094D 158.130 February 28, 2008 X 632.52 632.52 1,265.04 1,265.04 NELL66 Geoinformatics Exploration Canada Limited 24-Oct-06 544240 094D 172.480 February 28, 2008 X 689.92 689.92 1,379.84 1,379.84 NELL67 Geoinformatics Exploration Canada Limited 24-Oct-06 544259 094D 179.550 February 28, 2008 X 718.20 718.20 1,436.40 1,436.40 NELL68 Geoinformatics Exploration Canada Limited 24-Oct-06 544260 094D 172.380 February 28, 2008 X 689.52 689.52 1,379.04 1,379.04 NELL69 Geoinformatics Exploration Canada Limited 24-Oct-06 544279 094D 179.590 February 28, 2008 X 718.36 718.36 1,436.72 1,436.72 NELL70 Geoinformatics Exploration Canada Limited 24-Oct-06 544280 094D 143.680 February 28, 2008 X 574.72 574.72 1,149.44 1,149.44 NELL71 Geoinformatics Exploration Canada Limited 24-Oct-06 544281 094D 64.630 February 28, 2008 X 258.52 258.52 517.04 517.04 NELL72 Geoinformatics Exploration Canada Limited 28-Mar-07 555223 094C 448.780 March 28, 2008 X 1,795.12 1,795.12 3,590.24 3,590.24 NELL73 Geoinformatics Exploration Canada Limited 28-Mar-07 555224 094C 341.065 March 28, 2008 X 1,364.26 1,364.26 2,728.52 2,728.52 NELL74 Geoinformatics Exploration Canada Limited 28-Mar-07 555225 094C 269.260 March 28, 2008 X 1,077.04 1,077.04 2,154.08 2,154.08

earliest expiry TOTAL 248 claims hectares 101,324 February 28, 2008 0 405,295 405,295 810,590 810,590

sq. km 1,013acres 250,371

6 of 6 11/05/2007

Geoinformatics Exploration Canada LimitedKLIYUL Project Claim Listing Omineca Mining District, British Columbia

Claim Owner Issue Tenure NTS Map Area Expiry Yearly Assessment RequirementsName Date No. Number (hectares) 07 08 09 10 11

KLI No. 1 Kennecott Canada Exploration Inc. 10-Aug-70 245065 z 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 2 Kennecott Canada Exploration Inc. 10-Aug-70 245066 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 3 Kennecott Canada Exploration Inc. 10-Aug-70 245067 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 4 Kennecott Canada Exploration Inc. 10-Aug-70 245068 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 5 Kennecott Canada Exploration Inc. 10-Aug-70 245069 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 6 Kennecott Canada Exploration Inc. 10-Aug-70 245070 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 7 Kennecott Canada Exploration Inc. 10-Aug-70 245071 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 8 Kennecott Canada Exploration Inc. 10-Aug-70 245072 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 9 Kennecott Canada Exploration Inc. 10-Aug-70 245073 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 10 Kennecott Canada Exploration Inc. 10-Aug-70 245074 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 11 Kennecott Canada Exploration Inc. 10-Aug-70 245075 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 12 Kennecott Canada Exploration Inc. 10-Aug-70 245076 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 13 Kennecott Canada Exploration Inc. 10-Aug-70 245077 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 14 Kennecott Canada Exploration Inc. 10-Aug-70 245078 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 15 Kennecott Canada Exploration Inc. 10-Aug-70 245079 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 16 Kennecott Canada Exploration Inc. 10-Aug-70 245080 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 17 Kennecott Canada Exploration Inc. 10-Aug-70 245081 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 18 Kennecott Canada Exploration Inc. 10-Aug-70 245082 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 19 Kennecott Canada Exploration Inc. 10-Aug-70 245083 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 20 Kennecott Canada Exploration Inc. 10-Aug-70 245084 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 21 Kennecott Canada Exploration Inc. 11-Sep-70 245155 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 25 Kennecott Canada Exploration Inc. 11-Sep-70 245156 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 26 Kennecott Canada Exploration Inc. 11-Sep-70 245157 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 27 Kennecott Canada Exploration Inc. 11-Sep-70 245158 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI No. 28 Kennecott Canada Exploration Inc. 11-Sep-70 245159 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI #39 Kennecott Canada Exploration Inc. 12-Jul-71 245382 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI #40 Kennecott Canada Exploration Inc. 12-Jul-71 245383 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI #41 Kennecott Canada Exploration Inc. 12-Jul-71 245384 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI #42 Kennecott Canada Exploration Inc. 12-Jul-71 245385 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI #43 Kennecott Canada Exploration Inc. 12-Jul-71 245386 094D050 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI #44 Kennecott Canada Exploration Inc. 12-Jul-71 245387 094D050 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI #45 Kennecott Canada Exploration Inc. 12-Jul-71 245388 094D050 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI #46 Kennecott Canada Exploration Inc. 12-Jul-71 245389 094D050 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI #47 Kennecott Canada Exploration Inc. 12-Jul-71 245390 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI #48 Kennecott Canada Exploration Inc. 12-Jul-71 245391 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI #49 Kennecott Canada Exploration Inc. 12-Jul-71 245392 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI #50 Kennecott Canada Exploration Inc. 12-Jul-71 245393 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 UTA #4 Kennecott Canada Exploration Inc. 29-Aug-73 245777 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 UTA #6 Kennecott Canada Exploration Inc. 29-Aug-73 245778 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 UTA #8 Kennecott Canada Exploration Inc. 29-Aug-73 245779 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 YUL-7 Kennecott Canada Exploration Inc. 15-Jul-93 319492 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 YUL-8 Kennecott Canada Exploration Inc. 15-Jul-93 319493 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 YUL-9 Kennecott Canada Exploration Inc. 15-Jul-93 319494 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 YUL-10 Kennecott Canada Exploration Inc. 15-Jul-93 319495 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00

1 of 2 11/05/2007

Geoinformatics Exploration Canada LimitedKLIYUL Project Claim Listing Omineca Mining District, British Columbia

Claim Owner Issue Tenure NTS Map Area Expiry Yearly Assessment RequirementsName Date No. Number (hectares) 07 08 09 10 11

YUL-11 Kennecott Canada Exploration Inc. 15-Jul-93 319496 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 YUL-12 Kennecott Canada Exploration Inc. 20-Jul-93 319497 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 YUL-13 Kennecott Canada Exploration Inc. 20-Jul-93 319498 094D060 25 February 28, 2008 X 200.00 200.00 200.00 200.00 KLI 51 Geoinformatics Exploration Canada Limited 13-Apr-06 532002 094D/09 446.18 February 28, 2008 X 1,784.72 1,784.72 3,569.44 3,569.44 KLI 52 Geoinformatics Exploration Canada Limited 13-Apr-06 532005 094D/09 357.066 February 28, 2008 X 1,428.26 1,428.26 2,856.53 2,856.53 KLI 53 Geoinformatics Exploration Canada Limited 13-Apr-06 532011 094D/09 392.925 February 28, 2008 X 1,571.70 1,571.70 3,143.40 3,143.40 KLI 54 Geoinformatics Exploration Canada Limited 13-Apr-06 532014 094D/09 446.019 February 28, 2008 X 1,784.08 1,784.08 3,568.15 3,568.15 KLI 55 Geoinformatics Exploration Canada Limited 13-Apr-06 532015 094D/09 445.836 February 28, 2008 X 1,783.34 1,783.34 3,566.69 3,566.69 KLI 56 Geoinformatics Exploration Canada Limited 13-Apr-06 532020 094D/09 445.834 February 28, 2008 X 1,783.34 1,783.34 3,566.67 3,566.67 KLI 57 Geoinformatics Exploration Canada Limited 13-Apr-06 532028 094D/09 445.821 February 28, 2008 X 1,783.28 1,783.28 3,566.57 3,566.57 KLI 58 Geoinformatics Exploration Canada Limited 13-Apr-06 532079 094D/09 445.567 February 28, 2008 X 1,782.27 1,782.27 3,564.54 3,564.54 KLI 59 Geoinformatics Exploration Canada Limited 13-Apr-06 532080 094D/09 427.502 February 28, 2008 X 1,710.01 1,710.01 3,420.02 3,420.02 KLI 60 Geoinformatics Exploration Canada Limited 13-Apr-06 532081 094D/09 445.565 February 28, 2008 X 1,782.26 1,782.26 3,564.52 3,564.52 KLI 61 Geoinformatics Exploration Canada Limited 13-Apr-06 532082 094D/09 445.551 February 28, 2008 X 1,782.20 1,782.20 3,564.41 3,564.41 KLI 62 Geoinformatics Exploration Canada Limited 13-Apr-06 532083 094D/09 427.495 February 28, 2008 X 1,709.98 1,709.98 3,419.96 3,419.96 KLI 63 Geoinformatics Exploration Canada Limited 13-Apr-06 532084 094D/09 427.548 February 28, 2008 X 1,710.19 1,710.19 3,420.38 3,420.38 KLI 64 Geoinformatics Exploration Canada Limited 13-Apr-06 532085 094D/09 445.361 February 28, 2008 X 1,781.44 1,781.44 3,562.89 3,562.89 Geoinformatics Exploration Canada Limited 13-Apr-06 532086 094D/09 445.157 February 28, 2008 X 1,780.63 1,780.63 3,561.26 3,561.26 KLI 66 Geoinformatics Exploration Canada Limited 13-Apr-06 532087 094D/09 445.325 February 28, 2008 X 1,781.30 1,781.30 3,562.60 3,562.60 KLI 67 Geoinformatics Exploration Canada Limited 13-Apr-06 532089 094D/09 356.096 February 28, 2008 X 1,424.38 1,424.38 2,848.77 2,848.77 KLI 68 Geoinformatics Exploration Canada Limited 13-Apr-06 532090 094D/09 320.475 February 28, 2008 X 1,281.90 1,281.90 2,563.80 2,563.80 KLI 69 Geoinformatics Exploration Canada Limited 13-Apr-06 532091 094D/09 320.476 February 28, 2008 X 1,281.90 1,281.90 2,563.81 2,563.81 KLI 70 Geoinformatics Exploration Canada Limited 13-Apr-06 532092 094D/09 267.048 February 28, 2008 X 1,068.19 1,068.19 2,136.38 2,136.38 MES 1 Geoinformatics Exploration Canada Limited 25-Apr-06 533027 094D 429.325 February 28, 2008 X 1,717.30 1,717.30 3,434.60 3,434.60 MES 2 Geoinformatics Exploration Canada Limited 25-Apr-06 533030 094C 429.48 February 28, 2008 X 1,717.92 1,717.92 3,435.84 3,435.84 MES 3 Geoinformatics Exploration Canada Limited 25-Apr-06 533033 094D 429.546 February 28, 2008 X 1,718.18 1,718.18 3,436.37 3,436.37 MES 4 Geoinformatics Exploration Canada Limited 25-Apr-06 533034 094C 268.572 February 28, 2008 X 1,074.29 1,074.29 2,148.58 2,148.58 MES 5 Geoinformatics Exploration Canada Limited 25-Apr-06 533035 094D 268.576 February 28, 2008 X 1,074.30 1,074.30 2,148.61 2,148.61 MES 6 Geoinformatics Exploration Canada Limited 25-Apr-06 533036 094C 429.025 February 28, 2008 X 1,716.10 1,716.10 3,432.20 3,432.20 MES 7 Geoinformatics Exploration Canada Limited 25-Apr-06 533037 094C 411.321 February 28, 2008 X 1,645.28 1,645.28 3,290.57 3,290.57 MES 8 Geoinformatics Exploration Canada Limited 25-Apr-06 533038 094C 429.22 February 28, 2008 X 1,716.88 1,716.88 3,433.76 3,433.76 MES 9 Geoinformatics Exploration Canada Limited 25-Apr-06 533040 094C 214.53 February 28, 2008 X 858.12 858.12 1,716.24 1,716.24

earliest expiry TOTAL 76 claims hectares 12,683 April 13, 2007 0 55,434 55,434 101,468 101,468

sq. km 127acres 31,341

2 of 2 11/05/2007

Omineca Mining District, British ColumbiaClaim Owner Issue Tenure NTS Map Area ExpiryName Date No. Number (hectares) 07 08 09 10 11

Commander (ABE) Commander Resources Ltd. 514561 94C.031,32 1505.741 February 28, 2008 X 6,022.96 6,022.96 Commander Resources Ltd. 514577 94C.031,32 1129.927 February 28, 2008 X 4,519.71 4,519.71 Commander Resources Ltd. 514579 94C.032 717.404 February 28, 2008 X 2,869.62 2,869.62 ABE 9 Commander Resources Ltd. 501310 94C.031 448.219 February 28, 2008 X 1,792.88 1,792.88 ABE 10 Commander Resources Ltd. 501274 94C.031 430.485 February 28, 2008 X 1,721.94 1,721.94 ABE11 Commander Resources Ltd. 501313 94C.031 125.54 February 28, 2008 X 502.16 502.16

6 4,357.32 17,429.26 17,429.26 Commander (PAL)PAL 1 Commander Resources Ltd. 518338 94C.023 449.13 February 28, 2008 X 1,796.52 1,796.52 PAL 2 Commander Resources Ltd. 518335 94C.023 269.597 February 28, 2008 X 1,078.39 1,078.39 PAL 3 Commander Resources Ltd. 518330 94C.023 89.826 February 28, 2008 X 359.30 359.30 PAL 4 Commander Resources Ltd. 518333 94C.023 53.919 February 28, 2008 X 215.68 215.68 PAL 5 Commander Resources Ltd. 501205 94C.023 269.448 February 28, 2008 X 1,077.79 1,077.79

5 1,131.92 4,527.68 4,527.68 Commander (TUT)TUT 1 Commander Resources Ltd. 501480 94C.022 197.574 February 28, 2008 X 790.30 790.30 TUT 2 Commander Resources Ltd. 501440 94C.022 161.645 February 28, 2008 X 646.58 646.58

2 359.22 1,436.88 1,436.88 Commander (TUT South)TUT 4 Commander Resources Ltd. 501366 94C.022 431.459 February 28, 2008 X 1,725.84 1,725.84 TUT 5 Commander Resources Ltd. 504697 94C.022 431.318 February 28, 2008 X 1,725.27 1,725.27

2 862.78 3,451.11 3,451.11 Commander (MATE)MATE 1 Commander Resources Ltd. 501566 94C.022 431.859 February 28, 2008 X 1,727.44 1,727.44 MATE 2 Commander Resources Ltd. 501632 94C.022,23 431.856 February 28, 2008 X 1,727.42 1,727.42 MAT Commander Resources Ltd. 518781 94C.022,23 143.991 February 28, 2008 X 575.96 575.96

3 1,007.71 4,030.82 4,030.82 Commander (ATEN)ATEN Commander Resources Ltd. 501473 94C.013,23 432.057 November 4, 2008 X 1,728.23 1,728.23 ATEN 2 Commander Resources Ltd. 504735 94C.013,23 432.167 November 4, 2008 X 1,728.67 1,728.67 ATEN 3 Commander Resources Ltd. 527312 94C.013,23 432.188 February 28, 2008 X 1,728.75 1,728.75 ATEN 4 Commander Resources Ltd. 527316 94C.013 432.387 February 28, 2008 X 1,729.55 1,729.55 ATEN 5 Commander Resources Ltd. 527318 94C.013 432.38 February 28, 2008 X 1,729.52 1,729.52 ATEN 6 Commander Resources Ltd. 527319 94C.013 396.191 February 28, 2008 X 1,584.76 1,584.76 ATEN 7 Commander Resources Ltd. 527321 94C.013,23 395.981 February 28, 2008 X 1,583.92 1,583.92 7 2,953.35 - 11,813.40 11,813.40

Commander TOTAL 25 10,672.29 - 42,689.16 42,689.16

Geoinformatics Exploration Canada LimitedCommander Option Claim Listing


Omineca Mining District, British ColumbiaClaim Owner Issue Tenure NTS Map Area ExpiryName Date No. Number (hectares) 07 08 09 10 11

Ringo Norwest Enterprises Inc. 528561 161.060 February 28, 2008 644.24 644.24 644.24 1,288.48 1,288.48 Starr Norwest Enterprises Inc. 528562 214.828 February 28, 2008 859.31 859.31 859.31 1,718.62 1,718.62 KC Norwest Enterprises Inc. 532828 428.659 February 28, 2008 1,714.64 1,714.64 1,714.64 3,429.27 3,429.27 PGE Norwest Enterprises Inc. 533639 447.670 February 28, 2008 1,790.68 1,790.68 1,790.68 3,581.36 3,581.36 Westend Norwest Enterprises Inc. 533724 125.334 February 28, 2008 501.34 501.34 501.34 1,002.67 1,002.67 Eastside Norwest Enterprises Inc. 533727 161.062 February 28, 2008 644.25 644.25 644.25 1,288.50 1,288.50 Bingo Norwest Enterprises Inc. 551350 357.287 February 7, 2007 1,429.15 1,429.15 1,429.15 2,858.30 2,858.30 1 More Bango Norwest Enterprises Inc. 551355 17.867 February 7, 2007 71.47 71.47 71.47 142.94 142.94 Two More BingNorwest Enterprises Inc. 551360 35.738 February 7, 2007 142.95 142.95 142.95 285.90 285.90 MES 10 Norwest Enterprises Inc. 551538 35.715 February 9, 2007 142.86 142.86 142.86 285.72 285.72

earliest expiryTOTAL 10 claims hectares 1,985 February 6, 2007 7,941 7,941 7,941 15,882 15,882

sq. km 20acres 4,905

Geoinformatics Exploration Canada LimitedNorwest (Hamel) Option Claim Listing

29

Appendix 2: Stream sediment sample location sites and assay

certificates

SampleID Coordinate System Easting Northing Cu_ppm Au_ppb Ag_ppm Mo_ppm Pb_ppm Zn_ppm411751 NAD83_UTM_10 342998 6221450 109.75 6.4 0.239 3.73 3.74 36.9411752 NAD83_UTM_10 343979 6221020 139.81 8.4 0.189 5.45 6.78 59.1411753 NAD83_UTM_10 344974 6221359 115.43 2.2 0.082 7.46 2.41 27.4411754 NAD83_UTM_10 345820 6219390 514.23 33.6 0.305 9.59 18.72 114.3411755 NAD83_UTM_10 346384 6220577 259.42 6.3 0.145 4.2 8.34 70.4411756 NAD83_UTM_10 346143 6220443 521.61 13.3 0.264 4.41 17.57 104411758 NAD83_UTM_10 346393 6221317 149.19 5.5 0.167 5.36 3.67 28.3411759 NAD83_UTM_10 348732 6222337 68.65 4.4 0.055 3.46 2.82 32.7411760 NAD83_UTM_10 349230 6222218 167.88 4.1 0.252 1.62 3.7 45.5411761 NAD83_UTM_10 349731 6221836 253.04 3 0.382 1.1 5.11 64.1411762 NAD83_UTM_10 350102 6222251 107.59 2.8 0.121 7.92 3.63 34411763 NAD83_UTM_10 345816 6223655 156.24 5.1 0.073 3.99 9.35 61.5411764 NAD83_UTM_10 345769 6223546 165.84 11.6 0.069 3.59 7.38 60.6411765 NAD83_UTM_10 347639 6224674 127.16 2.6 0.072 6.02 8.44 89411766 NAD83_UTM_10 349678 6224637 108.8 2.7 0.092 2.9 5.68 65411767 NAD83_UTM_10 350168 6224621 103.63 1.3 0.045 2.05 4.95 71.4411769 NAD83_UTM_10 346198 6226658 173.36 5.3 0.135 11.63 11.51 84.5411770 NAD83_UTM_10 347088 6228515 141.73 7.9 0.198 0.92 7.2 169411771 NAD83_UTM_10 347174 6229556 100.52 13.5 0.204 3.12 8.37 109411772 NAD83_UTM_10 345018 6229920 173.14 7.6 0.499 0.87 4.59 129.5411773 NAD83_UTM_10 342953 6228161 147.76 2.4 0.23 4.38 6.4 70.8411774 NAD83_UTM_10 342844 6226143 159.69 20.5 0.306 4.33 8.56 67.8411775 NAD83_UTM_10 342342 6223473 217.51 33.6 0.38 5.92 10.39 116411776 NAD83_UTM_10 342242 6225126 333.77 13.5 1.119 12.02 33.91 70.4411777 NAD83_UTM_10 342235 6225123 235.32 48.2 0.267 16.68 11.73 70.4411778 NAD83_UTM_10 340856 6224585 153.67 6.1 0.153 9.66 10.38 76.6411779 NAD83_UTM_10 339375 6228990 250.66 6.1 0.229 5.79 11.31 71.5411780 NAD83_UTM_10 339726 6229407 129.16 5.6 0.114 2.02 6.89 59.9411781 NAD83_UTM_10 340254 6230517 132.22 5 0.077 2.34 3.67 54.7411782 NAD83_UTM_10 340254 6230517 130.75 12.4 0.089 2.23 3.9 54.6411783 NAD83_UTM_10 340239 6230325 115.85 5.7 0.116 4.13 4.23 53.6411784 NAD83_UTM_10 341215 6232070 84.15 4.7 0.201 3.55 2.17 21.8411785 NAD83_UTM_10 341936 6233141 55.2 315.3 0.092 1.36 2.99 50.7411786 NAD83_UTM_10 338470 6231086 95.3 2.9 0.073 4.6 4.1 50.4411787 NAD83_UTM_10 336893 6231198 173.96 12.4 0.13 2.78 6.59 68.4411788 NAD83_UTM_10 336210 6229216 133.11 14.8 0.079 4.47 5.67 75.1411789 NAD83_UTM_10 333246 6231298 316.15 11.3 0.114 2.41 4.32 65.8411790 NAD83_UTM_10 333219 6234705 94.02 2.4 0.062 2.92 3.61 40.8

SampleID Coordinate System Easting Northing Cu_ppm Au_ppb Ag_ppm Mo_ppm Pb_ppm Zn_ppm411791 NAD83_UTM_10 330729 6234760 208.53 7.9 0.305 4.21 12.73 101.1411792 NAD83_UTM_10 333704 6235791 69.95 2.2 0.206 1.4 16.24 42.3411793 NAD83_UTM_10 336581 6237672 110.61 85.8 0.197 0.51 4.03 171.3411794 NAD83_UTM_10 338118 6238383 79.19 4.1 0.134 2.02 5.69 121.4411795 NAD83_UTM_10 341671 6239034 181.03 9 0.337 3.23 7.21 463.8411796 NAD83_UTM_10 343388 6238963 144.06 256.7 0.229 1.05 7.4 67.3411797 NAD83_UTM_10 343388 6238963 142.61 59.6 0.156 1.12 7.66 80.8411798 NAD83_UTM_10 342484 6238168 102.76 1.5 0.263 1.21 15.7 151.5411799 NAD83_UTM_10 338129 6234596 72.36 20 0.072 1.76 1.84 28.5411800 NAD83_UTM_10 338181 6234432 104.36 5.4 0.088 1.5 2.86 34.9411801 NAD83_UTM_10 343403 6221058 66.28 5.2 0.269 5.64 3.38 42.2411802 NAD83_UTM_10 344554 6221069 121.27 3.7 0.174 6.49 4.09 58.9411803 NAD83_UTM_10 345002 6221119 257.2 602.9 0.317 3.09 8.19 67.7411804 NAD83_UTM_10 346575 6220106 478.65 42.9 0.326 8.11 16.32 108.6411805 NAD83_UTM_10 347603 6220419 187.13 10 0.108 8.24 6.66 58.5411806 NAD83_UTM_10 348325 6221891 159.14 2.2 0.068 9.37 4.5 75.4411807 NAD83_UTM_10 349100 6221062 200.91 3.8 0.287 2.75 5.03 78.6411808 NAD83_UTM_10 348994 6221137 164.63 4.4 0.214 5.95 4.6 65.5411809 NAD83_UTM_10 349451 6220923 218.16 5.6 0.255 2 4.52 44.3411810 NAD83_UTM_10 350158 6220776 149.67 3.5 0.149 5.34 4.64 63411811 NAD83_UTM_10 346655 6223126 138.6 4.1 0.103 5.36 3.48 41.4411812 NAD83_UTM_10 348282 6224293 111.03 1.9 0.087 3.57 8.19 99.6411813 NAD83_UTM_10 349094 6224490 146.49 6.9 0.108 5.41 8.11 111.3411814 NAD83_UTM_10 349068 6224581 124.74 5.4 0.103 9.34 8.6 129.7411815 NAD83_UTM_10 349993 6227404 79.43 8.5 0.12 0.56 5.3 110.2411816 NAD83_UTM_10 349818 6227397 131.37 7.1 0.128 1.14 10.22 107.1411817 NAD83_UTM_10 348308 6227525 122.53 6.4 0.156 0.76 12.65 195.8411818 NAD83_UTM_10 348170 6227541 138.11 9.8 0.213 0.67 24.23 195411819 NAD83_UTM_10 347879 6229368 130.37 6.3 0.311 1.57 19.57 224.2411820 NAD83_UTM_10 348424 6230441 51.06 8.3 0.088 1.95 2.99 86411821 NAD83_UTM_10 345863 6230227 115.91 5.1 0.13 4.34 6.22 103.9411822 NAD83_UTM_10 344661 6229684 107.7 1.2 0.204 4.37 7.23 72.7411823 NAD83_UTM_10 344685 6229628 134.92 3.9 0.172 3.14 6.14 65411824 NAD83_UTM_10 344088 6229173 265.9 5.4 0.304 3.65 12.66 83411825 NAD83_UTM_10 348424 6230441 55.76 165.8 0.146 1.86 2.93 86.6411826 NAD83_UTM_10 340990 6226380 161.86 8.5 0.215 7.53 9.55 74.4411827 NAD83_UTM_10 341505 6224743 146.01 3 0.161 8.7 5.2 45.3411828 NAD83_UTM_10 338457 6227323 126.72 4.9 0.103 3.07 8.91 91.8

SampleID Coordinate System Easting Northing Cu_ppm Au_ppb Ag_ppm Mo_ppm Pb_ppm Zn_ppm411829 NAD83_UTM_10 338310 6227261 219.08 7.8 0.117 6.03 5.77 62.8411830 NAD83_UTM_10 338149 6227336 157.6 11.8 0.144 3.24 8.56 99.4411831 NAD83_UTM_10 341341 6229180 89.1 3.7 0.131 2.87 5.53 75.4411832 NAD83_UTM_10 333320 6232357 64.18 5.5 0.042 0.49 2.08 28.4411833 NAD83_UTM_10 341681 6230766 143.96 1.9 0.173 5.56 6.55 80.5411834 NAD83_UTM_10 342956 6232095 184.73 12.9 0.257 1.38 10.71 211.5411835 NAD83_UTM_10 344550 6233395 178.37 16.8 0.529 4.12 25.65 192.4411836 NAD83_UTM_10 335860 6229157 152.6 9.7 0.104 4.37 8.13 77.2411837 NAD83_UTM_10 335893 6229247 133.63 6.1 0.06 2.73 4.31 57.9411838 NAD83_UTM_10 333279 6233479 74.05 3.4 0.047 2.88 2.6 31.5411839 NAD83_UTM_10 334245 6235560 125.11 19.8 0.126 2.57 4.68 44.9411840 NAD83_UTM_10 335584 6237125 214.04 47.9 0.247 1.84 6.37 88411841 NAD83_UTM_10 336680 6237927 105.57 4.7 0.097 0.62 3.31 33.1411842 NAD83_UTM_10 339678 6236622 143.78 28.4 0.277 0.99 10.27 147.4411843 NAD83_UTM_10 339551 6236755 105.33 5.9 0.079 1.56 2.42 50.9411844 NAD83_UTM_10 338755 6235101 160.82 19.3 0.15 0.65 7.26 82411845 NAD83_UTM_10 338665 6235201 179.34 64.4 0.323 1.65 2.97 70411846 NAD83_UTM_10 337655 6233676 214.2 10.2 0.165 5.1 4.7 69.7411847 NAD83_UTM_10 337573 6233650 116.3 13.7 0.105 2.87 3.25 51.9411848 NAD83_UTM_10 337803 6234020 71.69 7.3 0.047 0.51 1.7 25.2411849 NAD83_UTM_10 341551 6241207 40.61 3 0.079 0.65 2.29 68.2411850 NAD83_UTM_10 341715 6240979 154.21 5.4 0.566 1.22 1.72 19.1411851 NAD83_UTM_10 336028 6240322 245.1 44.5 0.732 0.73 16.47 82.4411852 NAD83_UTM_10 336060 6240335 206.56 61.9 0.568 1 12.89 128.5411853 NAD83_UTM_10 336151 6241760 137.25 42.2 0.52 0.72 9.92 79.1411854 NAD83_UTM_10 338426 6242468 32.53 2.8 0.073 0.19 1.47 36.3411855 NAD83_UTM_10 337049 6243444 91.89 14.9 0.239 0.51 5.25 68411856 NAD83_UTM_10 335302 6242884 117.31 21 0.156 0.95 2.89 39.4411857 NAD83_UTM_10 332938 6242494 50.44 4 0.067 1.31 2.96 24.5411858 NAD83_UTM_10 332322 6242406 57.06 2.8 0.134 1.13 2.72 24.7411859 NAD83_UTM_10 332020 6241460 94.88 2.5 0.144 1.38 12.66 37.6411860 NAD83_UTM_10 335302 6242884 120.92 188.6 0.219 0.92 3.03 37.4411861 NAD83_UTM_10 328534 6240764 27.13 0.7 0.047 0.95 2.33 30.8411862 NAD83_UTM_10 330817 6242423 95.19 0.8 0.097 1.31 2.54 28.7411863 NAD83_UTM_10 330539 6242316 41.38 4.1 0.056 1.47 2.68 35.9411864 NAD83_UTM_10 319581 6248504 91.66 5.3 0.192 2.24 3.25 65.7411865 NAD83_UTM_10 318857 6249245 63.02 10.3 0.154 0.85 3.29 82.6411866 NAD83_UTM_10 322071 6249845 12.96 2.9 0.126 3.53 10.4 62.2

SampleID Coordinate System Easting Northing Cu_ppm Au_ppb Ag_ppm Mo_ppm Pb_ppm Zn_ppm411867 NAD83_UTM_10 324965 6251109 55.22 23.4 0.096 1.05 3.39 30.5411868 NAD83_UTM_10 320641 6253366 62.67 19.2 0.145 4.33 3.42 85.8411869 NAD83_UTM_10 319342 6254359 59.88 3.9 0.161 1.18 3.15 50.9411870 NAD83_UTM_10 318737 6254292 31.17 1.4 0.057 3.26 3.09 50.8411871 NAD83_UTM_10 317736 6254521 61.26 1.3 0.259 2.61 6.25 34.9411872 NAD83_UTM_10 317655 6254560 28.87 1.7 0.15 2.66 7.85 48.5411873 NAD83_UTM_10 316925 6253195 25.89 0.5 0.063 2.5 3.11 32.1411874 NAD83_UTM_10 315355 6251469 37.06 2.6 0.051 0.55 0.85 25411875 NAD83_UTM_10 323330 6261090 102.29 7.8 0.426 0.89 9.72 186.1411876 NAD83_UTM_10 323360 6261030 123.48 9.6 0.288 0.61 11.28 134.3411877 NAD83_UTM_10 323610 6261030 103.86 13.8 0.257 0.43 6.96 105.8411878 NAD83_UTM_10 324470 6261800 77.91 22.8 0.212 0.48 6.48 111.2411879 NAD83_UTM_10 325540 6260920 74.8 17.1 0.078 0.34 2.77 66.5411880 NAD83_UTM_10 327400 6235000 254.82 7.9 0.143 0.47 3.18 97.7411881 NAD83_UTM_10 327450 6235540 267.37 19.9 0.176 0.68 2.64 91.8411882 NAD83_UTM_10 327560 6235520 276.28 13.5 0.18 0.32 2.39 97.1411883 NAD83_UTM_10 326220 6228770 212.75 7.4 0.097 0.52 4.79 108.1411885 NAD83_UTM_10 322968 6258298 66.95 8.9 0.096 0.33 2.29 31.6411888 NAD83_UTM_10 327610 6250062 130.35 18.2 0.108 2.15 3.41 31.9411889 NAD83_UTM_10 327433 6249484 131.37 5.5 0.076 0.78 1.8 29.1411890 NAD83_UTM_10 325987 6249296 19.95 4.2 0.253 25.99 18.35 62.5411891 NAD83_UTM_10 326047 6249289 130.48 28.9 0.227 9.36 6.24 71.4411892 NAD83_UTM_10 324559 6245465 95.76 3.3 0.116 6.46 8.48 84.6411894 NAD83_UTM_10 334633 6250294 98.31 3 0.054 0.69 3.37 82.2411895 NAD83_UTM_10 332007 6250473 77.56 2.7 0.192 0.88 7.9 116.9411897 NAD83_UTM_10 315407 6256957 105.73 6.4 0.31 6.71 17.13 58.3411898 NAD83_UTM_10 315285 6257084 190.75 7.2 0.448 18.25 16.91 80.2411899 NAD83_UTM_10 313062 6256247 117.94 1.4 0.083 3.74 2.93 47.6411900 NAD83_UTM_10 344842 6236638 72.73 9.3 0.145 0.57 8.33 107.2411901 NAD83_UTM_10 340856 6241391 102.87 4.4 0.171 1.07 5.27 221.8411902 NAD83_UTM_10 340700 6241897 92.47 17.6 0.238 1.51 6.3 134.4411903 NAD83_UTM_10 339658 6242137 105.41 4.5 0.143 0.97 3.41 104411904 NAD83_UTM_10 334716 6239538 318.46 19.2 0.462 2.59 15.28 99.9411905 NAD83_UTM_10 339110 6242453 99.47 8 0.165 0.77 3.21 76.4411906 NAD83_UTM_10 338938 6242507 91.64 9.5 0.088 0.53 2.81 63411907 NAD83_UTM_10 335001 6240854 264.17 15.2 0.327 2.01 4.46 52.6411908 NAD83_UTM_10 332843 6239949 205.64 6.4 0.335 5.18 10.51 56.4411909 NAD83_UTM_10 332139 6238840 114.98 2.4 0.14 1.36 19.48 56.1

SampleID Coordinate System Easting Northing Cu_ppm Au_ppb Ag_ppm Mo_ppm Pb_ppm Zn_ppm411910 NAD83_UTM_10 332231 6240048 123.2 2.6 0.166 1.66 17.33 43.3411911 NAD83_UTM_10 332217 6240068 107.37 11.8 0.123 1.95 17.26 42.1411912 NAD83_UTM_10 332217 6240068 101.76 2.4 0.118 1.77 16.13 39.1411913 NAD83_UTM_10 330536 6241094 100.08 2.5 0.157 3 18.23 55.9411914 NAD83_UTM_10 328170 6240598 43.99 0.5 0.057 0.85 3.29 34.5411915 NAD83_UTM_10 328351 6243080 50.25 82.1 0.072 0.91 2.39 47411916 NAD83_UTM_10 326650 6243361 115.73 3.8 0.091 1.42 4.28 75.1411917 NAD83_UTM_10 333888 6243739 173.41 8.7 0.159 1.99 4.25 56.9411918 NAD83_UTM_10 319975 6247185 13.9 0.3 0.034 0.71 2.64 26.1411919 NAD83_UTM_10 320831 6248796 30.31 0.6 0.044 1.22 3.18 39411920 NAD83_UTM_10 321763 6249679 39.87 4.7 0.156 1.93 5.32 64.9411921 NAD83_UTM_10 325443 6252668 114.55 13.8 0.199 9.17 4.63 60.6411922 NAD83_UTM_10 318437 6250978 60.39 25.8 0.236 1.23 3.65 67.7411923 NAD83_UTM_10 318368 6252328 63.56 14.1 0.29 2.12 4.46 64.7411924 NAD83_UTM_10 318368 6252328 53.78 11.3 0.227 1.8 4.31 63.5411925 NAD83_UTM_10 318955 6254927 53.09 2 0.097 1.13 3.43 52.6411926 NAD83_UTM_10 318497 6254793 29.58 0.7 0.094 1.61 1.33 26.7411927 NAD83_UTM_10 315986 6251982 45.56 3 0.05 0.63 1.47 46.8411928 NAD83_UTM_10 315329 6248668 68.1 1.7 0.071 2.44 4.4 46.2411929 NAD83_UTM_10 316611 6246792 90.9 1.7 0.113 4.74 5.26 68.6411931 NAD83_UTM_10 325405 6258516 35.49 2.4 0.065 0.62 1.88 44.6411933 NAD83_UTM_10 320497 6254722 58.49 16.1 0.12 2.8 3.94 100411935 NAD83_UTM_10 328720 6249144 52.78 0.9 0.126 1.95 27.91 28411936 NAD83_UTM_10 329396 6249920 189.74 20.5 0.227 3.3 4.9 57.8411937 NAD83_UTM_10 323688 6246020 2.61 -0.2 0.029 4.46 4.06 29.4411940 NAD83_UTM_10 333321 6251242 85.09 443.7 0.156 0.83 5.22 80.1411941 NAD83_UTM_10 330693 6252059 74.64 5.5 0.151 0.51 5 79411942 NAD83_UTM_10 312612 6257424 33.83 1.9 0.026 0.27 1.97 26.3411943 NAD83_UTM_10 312595 6257392 109.58 1.8 0.063 1.79 1.42 39.3411944 NAD83_UTM_10 311340 6255623 108.17 2.5 0.117 6.53 4 53.9411945 NAD83_UTM_10 344552 6233405 156.3 14 0.416 5.41 21.98 162.8411946 NAD83_UTM_10 347298 6232597 147.02 12.5 0.178 1.19 8.38 84.7411947 NAD83_UTM_10 347321 6232597 113.85 20.2 0.142 1.38 12.99 115411948 NAD83_UTM_10 345403 6233413 135.55 55.7 0.341 2.41 11.12 175.8411949 NAD83_UTM_10 326474 6231802 108.52 1.2 0.078 1.28 1.21 53.9411950 NAD83_UTM_10 326292 6231394 139.68 1.8 0.067 0.88 1.96 71411951 NAD83_UTM_10 344052 6234372 403.17 5 0.239 9.17 3.03 50411952 NAD83_UTM_10 326385 6231397 55.6 0.9 0.102 1.97 3.48 56.9

SampleID Coordinate System Easting Northing Cu_ppm Au_ppb Ag_ppm Mo_ppm Pb_ppm Zn_ppm411953 NAD83_UTM_10 331245 6228647 108.97 5.7 0.151 0.9 3.9 89.2411954 NAD83_UTM_10 328553 6230897 265.19 8.3 0.211 0.92 2.91 98.2411955 NAD83_UTM_10 328600 6230907 158.64 4.5 0.077 0.56 1.72 79.2411956 NAD83_UTM_10 329175 6229352 136.22 8.6 0.094 0.48 2.1 73.5411957 NAD83_UTM_10 324630 6235462 196.56 3.3 0.094 1.61 2.28 97.6411958 NAD83_UTM_10 326935 6237716 175.57 6.8 0.148 1.78 2.8 104.4411959 NAD83_UTM_10 325669 6245436 92.9 17.2 0.141 6.68 5.52 89.4411960 NAD83_UTM_10 332182 6229947 126.95 7.7 0.152 1.15 4.28 73.6411961 NAD83_UTM_10 324547 6236456 148.94 3.1 0.091 0.63 2.05 70.6411962 NAD83_UTM_10 326319 6237363 284.47 9.4 0.158 1.28 2.57 119.3411963 NAD83_UTM_10 326326 6237356 78.79 35.4 0.097 1.85 4.19 59.3411964 NAD83_UTM_10 331090 6247665 181.24 361.7 0.37 0.94 7.01 75.5411965 NAD83_UTM_10 331910 6247667 105.14 22.7 0.147 2.29 14.15 31.6411966 NAD83_UTM_10 332400 6247676 62.14 4.3 0.085 0.66 9.86 93.7411967 NAD83_UTM_10 333981 6246656 97.33 13.6 0.072 1.13 4.27 87.6411968 NAD83_UTM_10 330271 6245235 152.4 46.4 0.206 0.99 3.46 44.6411969 NAD83_UTM_10 322468 6243417 5.37 -0.2 0.066 2.87 8.64 67411970 NAD83_UTM_10 323435 6242847 5.02 0.4 0.116 1.75 10.22 54.2411971 NAD83_UTM_10 330817 6247708 148.15 1.7 0.166 2.99 9.4 29.3411972 NAD83_UTM_10 330808 6247609 42.15 0.8 0.142 1.04 24.07 25.9411973 NAD83_UTM_10 332920 6247312 84.51 5.1 0.167 1.68 10.37 28.2411974 NAD83_UTM_10 333042 6247217 171.89 256 0.313 1.07 6.92 75.8411975 NAD83_UTM_10 333389 6247638 101.27 2.9 0.072 0.39 5.48 74.5411976 NAD83_UTM_10 328409 6246040 65.02 14.3 0.095 0.6 2.76 44411977 NAD83_UTM_10 324666 6241875 61.51 1.9 0.099 1.57 9.19 68.2411978 NAD83_UTM_10 310175 6259578 178.06 9.5 0.153 1.11 2.84 99.1411979 NAD83_UTM_10 313054 6255179 73.78 1.2 0.055 4.78 4.4 41.4411980 NAD83_UTM_10 314928 6255088 116.31 0.8 0.082 3.58 1.99 38411981 NAD83_UTM_10 317819 6251641 16.35 -0.2 0.056 4.85 4.01 45411982 NAD83_UTM_10 323260 6231593 44.16 0.3 0.039 2.06 6.91 38.2411983 NAD83_UTM_10 310548 6260591 126.76 5.1 0.105 1.11 2.59 63.6411984 NAD83_UTM_10 314783 6254542 130.62 0.9 0.103 3.03 2 60.4411985 NAD83_UTM_10 321377 6233335 104.25 2.2 0.056 1.08 1.9 43.6411986 NAD83_UTM_10 322602 6229010 13.66 -0.2 0.053 6.51 3.6 39411987 NAD83_UTM_10 322429 6229028 11.73 -0.2 0.061 1.77 2.62 41.6

30

Appendix 3: Kliyul diamond drill core logs, drill section and assay

certificates

KL06_30GEOINFORMATICS EXPLORATIONDRILL HOLE LOG

Geoinformatics Exploration Inc

KL06_30

Kliyul

325.37

NAD83_UTM_09

6265920.00

1775.00 m

Hole ended prematurely due to drill pad instability

GXL_KLIYUL_2006

DDHole ID

DataSet

Prospect

Hole type

Depth

Notes

Collar

m

12/08/2006Commenced

16/08/2006Completed

Hole ended prematurelyDrilling company

Tenement

Grid ID

Hole ended prematurelyGeologist

Hole ended prematurelySurvey Method

Easting

Northing

676486.00 RL

At Dip MethodAzimuth AzimuthID CommentsSurvey

81.40 -61.3230.6 CAMERANAD83_UTMm142.35 -61.8233.7 CAMERANAD83_UTMm203.30 -62.0230.1 CAMERANAD83_UTMm264.26 -62.4222.5 CAMERANAD83_UTMm325.22 -61.8226.0 CAMERANAD83_UTMm

LithologyFrom To Code GSize Text1 %

Logged by: Mclean_Trottm CommentsText2Qual Code GSize Text1 %Text2Qual

Lith 1 Lith 2

0.00 15.24 CASE 100

15.24 76.57 XSH F fr 100focl

76.57 78.97 IIO C fr 100cl

78.97 89.54 XSH F fr 100focl

89.54 90.60 IIO M fr 100cl

90.60 92.02 XSH F fr 100focl

92.02 96.92 YIAT F fr 100cl

96.92 99.40 XSH F fr 100focl

99.40 136.06 XSH F fo 100cl

136.06 136.89 VIAP F pp 100pp

136.89 159.94 XSH F fo 100cl

159.94 160.56 VIA F pp 100pp

160.56 239.80 XSH F fo 100cl

239.80 251.75 AQE F mx 100crat

KL06_30 10 May 2007 Page 1 of 13

251.75 277.28 XSH F 100cl

277.28 300.90 XSH F fo 100cl

300.90 302.27 III M cr 100lu

302.27 311.95 XSH F fo 100cl

311.95 321.42 XSH F 100cl

321.42 325.37 XSH F fo 100cl

LithologyFrom To

Logged by: Mclean_Trottm Description

0.00 15.24

15.24 76.57 Chloritic schist. Rock is a pale grayish-green, and is strongly crumbled and rubbly. Larger, more intact portions of core display a distinct schistosity/fabric, at a steep angle (nearperpendicular, although variable) to the core axis. Interval most likely represents an altered volcanic package (andesitic?), chloritized and strongly structurally modified. Primary textures/structures are difficult to detect, due to strong structural overprint. Fine-grained disseminated pyrite is ubiquitous, likely a function of the event that chloritized the rock animparted its fabric. Carbonate is seen locally. Local, paler patches of sericitic material observed, likely forming halos around later quartz veins.

76.57 78.97 Dioritic intrusive rock (?). Interval is altered in similar style to the overlying material (dominantly chloritized); however, this rock lacks fabric, and appears less fractured (more resto deformative processes). Relict dioritic textures are observed, although primary mineralogy has been overprinted extensively by alteration minerals.


89.54 90.60 Dioritic intrusive rock (?). Interval is altered in similar style to the overlying material (dominantly chloritized); however, this rock lacks fabric (possible very subtle fabric), and appeslightly less fractured (somewhat more resistant to deformative processes). Relict igneous textures are observed, although primary mineralogy has been overprinted extensively alteration minerals. Unit is finer grained, and texturally distinct from previous dioritic interval.


92.02 96.92 Andesitic tuff (?). This interval is generally fine-grained, pale grayish-green, and displays local clasts, generally subrounded to rounded. This unit has a weak fabric, and in all probability is chemically very similar to the surrounding rock. It is differentiated texturally, because in this case the texture is more or less preserved. The point being that there mno difference between this lithology and the surrounding rocks, other than the fact that this lithology is less altered for some reason.


99.40 136.06 Chloritic schist. Rock is a pale grayish-green, similar to the overlying chloritic schist except it is not rubbled- the core is relatively intact. Primary textures/structures have generalbeen overprinted and obliterated by metamorphic/structural fabric, although local relict textures are seen, including relict plagioglase phenocrysts. Unit is probably an altered volcpackage. Fabric is imparted by alignment of micas (predominantly chlorite), as well as common wispy gypsum veinlets in the same orientation. Fabric is not uniformly well develalthough it does dominate the interval. Local, restricted zones feature pale tan to whitish sericitic alteration overprinting the chloritic alteration (blue-green).

136.06 136.89 Plag-phyric Andesite. Rock is well preserved compared to the surrounding altered volcanics (late?). Plagioclase phenocrysts, altered to chlorite, are still readily visible. This rocnot feature a fabric. The dark (nearly mafic) character of the groundmass of this rock makes it difficult to ascertain to what degree the rock has been chloritized. Gypsum veiningpresent in this rock.

136.89 159.94 Chloritic schist. Rock is a pale grayish-green. Primary textures/structures have generally been overprinted and obliterated by metamorphic/structural fabric, although local relict textures are seen, including relict plagioglase phenocrysts. Unit is probably an altered volcanic package, with possible lesser amounts of altered dyke material. Fabric is impartealignment of micas (predominantly chlorite), as well as common wispy gypsum veinlets in the same orientation. Fabric is not uniformly well developed, although it does dominateinterval. Local, restricted zones feature pale tan to whitish sericitic alteration overprinting the chloritic alteration (blue-green).

159.94 160.56 Andesitic dyke. Rock is less altered than surrounding rock, although plagioclase phenocrysts have been ubiquitously epidotized. Rock appears to be relatively un-chloritized.

KL06_30 10 May 2007 Page 2 of 13

AlterationFrom To Alt1 Style Int.m CommentsAlt2 Style Int. Alt3 Style Int.Total Int.

15.24 76.57 CH pv STG The most prominent alteration observed in this interval is pervasive chlorite. Lesser amounts of sericitic alteration are present, overprinting chloritic, probably associated witlate veining. Clay is present locally. Trace epidote present locally.

SR pv MOD CY pv WKSTG

76.57 78.97 CH pv STG Rock is chloritized as above. Plagioclase phenocrysts have largely been altered to epidand/or clay.

EZ rep MOD CY pv WKSTG

78.97 99.40 CH pv STG The most prominent alteration observed in this interval is pervasive chlorite. Lesser amounts of sericitic alteration are present, overprinting chloritic, probably associated witlate veining. Clay is present locally. Trace epidote present locally.

SR pv MOD CY pv WKSTG

99.40 123.16 CH pv STG Rock is chloritized as above. Rock is ubiquitously veined with wispy, en echelon veinletof a soft, white material (sericite/clay?). Pervasive chlorite has been overprinted by pervasive sericite (?) locally, generally in conjunction with quartz veinlets.

EZ vsel MOD CY pv TRSTG

123.16 123.42 SR pv STG Sericitic altered zone. Lesser silica, possible clays.CY pv WK SL pv MODSTG123.42 128.43 CH pv STG Rock is chloritized pervasively. Plagioclase phenocrysts have largely been altered to

epidote and/or clay. Gypsum veinlets ubiquitous.EZ rep WK GP vsel WKSTG

128.43 129.27 SR pv STG Sericitic altered zone. Lesser silica, possible clays. Alteration is probably related to latequartz veins.

SL pv WK CY pv TRSTG

129.27 136.06 CH pv STG Rock is chloritized pervasively. Plagioclase phenocrysts have largely been altered to epidote and/or clay. Gypsum veinlets ubiquitous.

EZ rep WK GP vsel WKSTG

136.06 136.89 CH rep WK Lesser altered zone. Dominant alteration consists of chlorite replacement of plagioclasephenocrysts.

WK

136.89 140.76 CH pv STG Rock is chloritized pervasively. Plagioclase phenocrysts have largely been altered to epidote and/or clay. Gypsum veinlets ubiquitous.

EZ rep TR GP vsel WKSTG

140.76 141.85 SR pv STG Mixed alteration zone. Alteration grades between chloritic and sericitic (sericite generaladjacent to quartz veins). Lesser silicification associated with sericite.

CH pv MOD SL pv WKSTG

160.56 239.80 Chloritic schist. Rock is a pale grayish-green. Primary textures/structures have generally been overprinted and obliterated by metamorphic/structural fabric, although local relict textures are seen, including relict plagioglase phenocrysts. Unit is probably an altered volcanic package, with lesser amounts of possible altered dyke material. Fabric is impartealignment of micas (predominantly chlorite), as well as common wispy gypsum veinlets in the same orientation (emplaced through fabric?). Fabric is not uniformly well developedalthough it does dominate the interval. Local, restricted zones feature pale tan to whitish sericitic alteration overprinting the chloritic alteration (blue-green). Local plagioclase-phtextures are well developed, wherein the plagioclase has been altered to epidote. The lower portion of the interval features thick bull quartz veins, mineralized with pyrite (+/- chalcopyrite). Two such veins are noted from 223.63 to 225.21 m, and from 238.12 to 239.8 m. The rock surrounding these veins appears to have been silicified, sericitized, andpyritized to varying degrees (QSP), overprinting the chloritic alteration. The lower portion of the interval is also characterized by a decreased abundance of gypsum veining, althofabric is still strongly visible due to alignment of chlorite and sericite banding.

239.80 251.75 Quartz-sericite-pyrite- altered rock. Likely a volcanic protolith- impossible to be sure due to absence of relict textures/structures. Rock is pale tan, siliceous, and speckled with disseminated pyrite. A very subtle alignment is suggested in places. Gypsum veining rare. At least two phases of quartz veining are present- an early, narrow smoky quartz veiphase, and a late, thick, milky quartz phase (+/- sulphides). One of these quartz-veining episodes may have catalyzed the QSP alteration.

251.75 277.28 Chloritic schist. Rock is pervasively chloritized. Fabric is poorly developed in this interval. This unit is termed a schist for the sake of consistency, since texturally it is very differefrom the previous chloritic schists, but mineralogically it is identical. Locally, relict igneous textures are preserved. The lower portion of the interval has portions of well preservedporpyritic texture.

277.28 300.90 Cholritic schist. Fabric more strongly developed, fewer relict textures. Gypsum veining is rare.

300.90 302.27 Monzodioritic dyke, interval is tan in colour, comprised mainly of feldsapr with altered mafic minerals disributed evenly throughout. These mafic minerals (chloritized?) are suddenalighed at a high angle to the core axis.


311.95 321.42 Chloritic schist. Rock is pervasively chloritized. Fabric is poorly developed in this interval. This unit is termed a schist for the sake of consistency, since texturally it is very differefrom the previous chloritic schists, but mineralogically it is identical. Locally, relict igneous textures are preserved.


KL06_30 10 May 2007 Page 3 of 13

141.85 149.59 CH pv STG Alteration is dominated by pervasive chloritization. Local intersections of sericitic alteration, in conjunction with late quartz veins. Minor replacement of plagioclase with epidote.

SR pv WK EZ rep TRSTG


SL pv WK CH pv WKSTG

150.26 154.82 CH pv STG Pervasively chloritized rock. Sericite/clay veins are rare in this interval. Some silicificatiis at work in this interval. Local epidote replacement of plagioclase.

SL pv MOD EZ rep TRSTG


SL pv WK CY pv TRSTG

155.28 159.94 CH pv STG Pervasively chloritized rock. Sericite/clay veins are rare in this interval. Some silicificatiis at work in this interval. Local epidote replacement of plagioclase.

SL pv MOD EZ rep TRSTG

159.94 160.56 EZ rep MOD Weak to moderately altered interval (late?). Epidote replacing plagioclase phenocrysts, rare epidote veinlets.

MOD

160.56 173.30 CH pv STG Pervasively chloritized and silicified interval. Gypsum veinlets are seen commonly, as was local epidote veining.

SL pv MOD EZ vsel WKSTG

173.30 175.20 EZ rep MOD Moderately altered interval (late?). Epidote replacing plagioclase phenocrysts, rare epidveinlets. Dyke appears silicified.

SL pv MODMOD

175.20 181.69 CH pv STG Pervasively chloritized and silicified interval. Gypsum veins are seen commonly, as weas local epidote veining.

SL pv MOD EZ vsel TRSTG

181.69 223.21 CH pv MOD Rock is altered similarly to overlying interval. Interval is darker in colour (less silicificatioLess chloritization?) but is still nearly ubiquitously gypsum veined. Epidote veining/replacement is commonplace, particularly towards the top of the interval. Local pervasive sericitic overprint, associated with quartz veins.

EZ rep WK GP vsel MODSTG

223.21 237.25 SR pv MOD Rock is variably altered, containing banding of chloritic alteration overprinted (?) by quarsericite-pyrite alteration.

CH pv MOD SL pv MODSTG

237.25 251.75 SL vsel MOD Interval features strong quartz-sericite-pyrite (QSP) alteration. Abundance of quartz veiin this interval may be related to alteration.

SR pv STGSTG

251.75 325.37 CH pv STG Dominant alteration style in this interval is pervasive chlorite.STG

VeiningFrom To Vein1 Style Int.m Av. thick

(mm)Vein2 Style Int. Av. thick


(mm)Av.

AngleAv.

AngleAv.

AngleComments

15.24 99.40 ZVC WSP 15 0.3 15 The most readily apparent vein type in this interval is wispy calcite veining, cutting the fabric of the rock (late veining). This veining needs to be considered with a degree of caution, since veining is difficult to detect in the more rubbly portions of core, and is basically hypothetical in these portions, inferred by examining less broken segments of core (with the assumption that the veining is more or less consistenthroughout, regardless of the structural integrity of therock).

99.40 136.06 ZVO WSP 20 0.2 ZVQC FRV 20 0.5 ZVQ FRV 2.5 0.565 15 Dominant vein type in this interval is gypsum veinletsrunning parallel to fabric. Lesser amounts of quartz-carbonate-pyrite veins are observed. Quartz veins with associated pyrite and chalcopyrite are seen in thlower portion of the interval. Sulphides seem to anastomoze outward from the veins, hosted by associated microfractures.

136.06 136.89 ZVQC FRV 5 0.8 5 Interval is poorly veined, featuring quartz-carbonate veining (late).

KL06_30 10 May 2007 Page 4 of 13

136.89 150.26 ZVO WSP 20 0.2 ZVQC FRV 20 0.5 ZVQ FRV 2.5 0.565 15 Dominant vein type in this interval is gypsum veinletsrunning parallel to fabric. Lesser amounts of quartz-carbonate-pyrite veins are observed. Quartz veins with associated pyrite and chalcopyrite are seen locally.

150.26 164.85 ZVQC FRV 10 0.5 10 Interval is characterized by lack of en echelon gypsumveins. Veining observed is basically permutations of quartz-carbonate-epidote-pyrite.

164.85 173.30 ZVO WSP 20 0.2 ZVQC FRV 20 0.565 Dominant vein type in this interval is gypsum veinletsrunning parallel to fabric. Lesser amounts of quartz-carbonate-pyrite veins are observed.

173.30 175.20 ZVE FRV 1.5 0.4 ZVQC FRV 1.5 0.3 Very little veining present in this interval.

175.20 188.35 ZVO WSP 20 0.2 ZVQ FRV 20 0.8 ZVE 1 0.365 Dominant vein type in this interval is gypsum veinletsoriented relatively uniformly, imparting a fabric to the rock. Lesser amounts of quartz veinlets are observed

188.35 198.00 ZVE FRV 7 0.2 ZVQC FRV 7 0.25 ZVQ FRV 1.5 130 80 Gypsum veining is no longer observed. Instead, epidote veining has become more commonplace. Minor quartz-carbonate and quartz-pyrite veining.

198.00 223.63 ZVO WSP 15 0.2 ZVQC FRV 15 0.3 Gypsum veining ubiquitous. This vein type is more irregular, and the trending is more subtle.

223.63 225.21 ZVQ FRV 70 15 70 Intensely quartz-veined zone. Subordinate pyrite.

225.21 237.25 ZVQ FRV 5 0.85 ZVO WSP 5 0.3 Veining in this interval is dominated by quartz-feldspar. Gypsum veins are present, in minor quantitites.

237.25 239.80 ZVQ FRV 85 40 85 Interval dominated by thick milky quartz veins (+/- pyrite).

239.80 277.28 ZVQ FRV 5 3 ZVO WSP 5 0.2 ZVQ FRV 2.5 0.8 Most dominant vein type is quartz veining- several different phases are seen (at least two), consisting of early smoky quartz veins, and late milky quartz veinsMinor gypsum veining locally.

277.28 325.37 ZVQ FRV 5 2 ZVE WSP 5 0.2 Wispy epidote veinig is ubiquitous. Magneite +/- qtz veining is commonplace.

Mineralisation PercentFrom To CCP

Frac CCP Vein

PYDiss

PYFrac

PYOXFrac

PYVein

MAL Frac

CCP Diss

Description

15.24 76.57 0.05 1 0.05 Interval is characterized by abundant disseminated pyrite, related either to the structurometamorphic evthat chloritized the rock or to the structural event that shattered the overlying rock. Trace chalcopyrite disseminations observed locally. Pyrite is seen locally hosted by carbonate veins (+/- quartz).

76.57 78.97 Weakly mineralized zone. Coincidence of higher degree of structural integrity implies that pyrite mineralization is related to the structural event that shattered the overlying rock (ie more strongly fracturrock seems to contain more pyrite).

78.97 99.40 0.05 0.9 0.05 Interval is characterized by abundant disseminated pyrite, related either to the structurometamorphic evthat chloritized the rock or to the structural event that shattered the overlying rock. Trace chalcopyrite disseminations observed locally. Pyrite is seen locally hosted by carbonate veins (+/- quartz).

99.40 119.88 0.1 0.8 Interval is distinguished by relative absence of disseminated pyrite and dominance of vein-hosted pyrite(quartz-carbonate veins). Chalcopyrite is seen in increased abundance.

KL06_30 10 May 2007 Page 5 of 13

119.88 122.16 0.5 0.8 0.3 Strongly mineralized zone. More favourable pyrite-chalcopyrite tenor. Mineralization appears to be maihosted by microfractures related to early quartz veins, which are in turn weakly mineralized.

122.16 132.80 0.05 0.2 0.4 Weakly (although ubiquitously) mineralized zone. Sulphides are generally confined to quartz veins, although minor disseminated sulphides are seen.

132.80 134.78 1 1 0.7 Best mineralized interval seen up until this point. Mineralization appears to be mainly hosted by microfractures related to early quartz veins, which are in turn weakly mineralized. Interval is siliceous (correlation between mineralization and silicification?).

134.78 136.06 0.05 0.15 0.3 Weakly mineralized interval.136.89 137.50 0.6 0.4 0.8 Relatively strongly mineralized interval. Mineralization style as noted previously. Host rock is silicified

(correlation between silicification and mineralization?)137.50 140.00 0.2 0.2 0.6 Lesser mineralized zone, although chalcopyrite is still readily visible.140.00 157.98 0.08 0.14 0.5 Interval is poorly mineralized, with the exception of rare, localized veins containing significant chalcopyr

(see 148.13 m).157.98 159.94 0.3 0.8 0.4 Interval is relatively well mineralized, dominated by disseminated mineralization. Rock is siliceous.160.56 169.09 0.05 0.2 0.3 Interval is weakly (although ubiquitously) mineralized.169.09 170.34 0.25 1.25 Better mineralized zone. Relatively favourable py:cpy ratio.170.34 173.30 0.05 0.15 0.6 Weakly mineralized interval.175.20 191.20 0.05 0.45 0.3 Weakly mineralized interval. Both disseminated and vein-style mineralization is seen. 191.20 223.63 0.1 0.3 0.7 Mineralization in this interval is commonly observed in quartz veins. Rare magnetite veinlets are genera

sulphide-bearing. A narrow magnetite-chalcopyrite-pyrite veinlet is noted at 191.33 m. Possible molybdenite observed at 219.61 m, hosted by a milky quartz vein with associated chalcopyrite.

223.63 237.25 0.1 1 0.4 Mineralization in this interval is dominated by disseminated pyrite, seen mainly in the pale, tan-colouredsericitic material, and in lower concentration in the more chloritic material. Minor vein-style mineralizatiohosted by quartz veins.

237.25 239.80 0.1 0.5 Large, weakly mineralized milky quartz vein. Lower overall sulphide content, but more favourable pyrite:chalcopyrite ratio.

239.80 251.75 0.1 1.8 0.2 Large interval of disseminated pyrite mineralization. Pyrite is a component of pervasive QSP alteration.251.75 305.30 0.04 0.4 0.36 Interval of mixed mineralization. Disseminated pyrite seems to correspond with sericitic intersections. A

chalcopyrite is hosted by veins, intergrown with pyrite. Locally, epidote veins host significant chalcopyrit305.30 307.70 0.07 0.4 1 Interval is characterized by abundant vein hosed pyrite, associated qtz veins.307.70 317.02 0.04 0.4 0.36 Weakly mineralised zone.317.02 317.90 0.07 0.4 1 Sericitic zone with abundant pyrite.317.90 325.37 0.04 0.4 0.36 Variably mineralised zone

StructureFrom To Int.m Struct 1 DescriptionAngle Int.Struct 2 Angle Int.Struct 3 Angle

15.24 49.20 SFS STG Interval features a schistosity derived from alignment of micas. Overprinting this schistosity, thecore is strongly broken and rubbled (brittle shearing?).

ZRO STG

49.20 50.50 ZFG INT Interval is characterized by abundant clay (gouge?)- core is crumbled almost to a powder in places.


ZRO STG

76.57 78.97 ZRO MOD Interval is characterized by relative lack of fabric, and lesser degree of fracturing (more competlithology).


ZRO STG

99.40 136.06 SFS MOD Interval is relatively intact from a structural standpoint, although closed en echelon fracture vein(gypsum) is commonplace. Fabric is still present.

ZRO MOD

KL06_30 10 May 2007 Page 6 of 13

136.06 136.89 ZRO WK Interval is virtually pristine structurally.136.89 150.26 SFS MOD Interval is relatively intact from a structural standpoint, although closed en echelon fracture vein

(gypsum) is commonplace. Fabric is still present.ZRO MOD

150.26 159.94 ZRO MOD Fabric is weak to nonexistent here, seen in localized sericitic intersects. Minor fracture veining159.94 160.56 ZRO WK Interval has a high structural integrity. Weak fracture veining.160.56 164.85 ZRO MOD Fabric is weak to nonexistent here, seen in localized sericitic intersects. Minor fracture veining164.85 173.30 SFS MOD Relatively well developed fabric, created by aligned gypsum veinlets (en echelon).65 ZRO MOD173.30 175.20 ZRO WK Interval is relatively intact structurally, although in places is broken up somewhat.175.20 188.35 SFS MOD Relatively well developed fabric, created by aligned gypsum veinlets (en echelon).65 ZRO MOD188.35 223.21 SFS WK Fabric is somewhat more subtle in this interval, although closed fractures are still commonplaceZRO MOD223.21 239.80 SFS MOD relatively well developed fabric created by alignment of micas. Strong quartz fracture veining.ZRO STG239.80 277.28 SFS TR Fabric is weak, localized. Variable fracture veining.ZRO MOD277.28 311.95 SFS MOD Fabric is better developed.ZRO MOD311.95 321.42 SFS TR Fabric is weak, localized. Variable fracture veining.ZRO WK321.42 325.37 SFS MOD Fabric is better developed.ZRO MOD

Depth Beta Dip/Plunge

Feature Width DescriptionPoint Structure

AlphaDip/Plunge Dir.

m Gamma Reliability

109.34 178.0ZVO Narrow sericite/clay (?) veinlet, part of a widespread en echelon series of similar veins, which lethe rock a fabric overall.

0.2 55.0 high

109.87 287.0ZVQ quartz vein crosscutting fabric, hosting minor pyrite +/- chalcopyrite.0.5 50.0 high110.48 150.0ZVO Narrow sericite/clay (?) veinlet, part of a widespread en echelon series of similar veins, which le

the rock a fabric overall.0.2 65.0 high

112.48 288.0ZVQ Quartz vein with minor epidote and pyrite.0.8 53.0 high113.83 160.0ZVO Narrow sericite/clay (?) veinlet, part of a widespread en echelon series of similar veins, which le


114.91 258.0ZVQ quartz vein with trace pyrite0.6 45.0 high119.01 330.0ZVQ quartz vein with significant pyrite and chalcopyrite.1 45.0 high119.96 232.0ZVQ quartz vein with significant pyrite and chalcopyrite.2 68.0 high121.04 275.0ZVQ quartz vein with significant pyrite and chalcopyrite.2.5 55.0 high122.08 325.0ZVQ quartz vein with associated pyrite and chalcopyrite.0.5 32.0 high123.80 230.0ZVO Narrow sericite/clay (?) veinlet, part of a widespread en echelon series of similar veins, which le


126.05 0.0ZVQ Quartz vein with abundant pyrite and chalcopyrite. Vein is offset by several other fracture veins(therefore early).

2.5 90.0 high

127.23 0.0ZVQ Quartz vein with abundant pyrite. 0.6 85.0 high128.80 265.0ZVO Narrow sericite/clay (?) veinlet, part of a widespread en echelon series of similar veins, which le


130.45 330.0SFS Sericite altered zone.10 74.0 high132.91 310.0ZVQ Quartz vein containing a high concentration of chalcopyrite.1 58.0 high134.54 302.0ZVS Chalcopyrite rich vein, lesser quartz and pyrite.0.8 50.0 high136.06 295.0SCI Dyke contact0.05 60.0 high136.89 340.0SCI Dyke contact0.05 62.0 high137.30 310.0ZVQ Layered quartz vein with sulphide banding (pyrite>chalcopyrite).4 55.0 high138.20 278.0ZVQ Early quartz vein with abundant sulphides.0.7 75.0 high

KL06_30 10 May 2007 Page 7 of 13

139.00 280.0ZVQ Early quartz veined zone with abundant sulphides.4 55.0 high141.20 285.0SFS Sericite altered zone, features pyritic banding.12 55.0 high145.75 298.0ZVS Pyritic vein, with lesser quartz and sericitic selvage.0.8 43.0 high147.10 282.0ZVQ Thin quartz vein hosting pyrite, +/- epidote.0.6 22.0 high151.24 0.0ZVQ Quartz vein with minor chalcopyrite and pyrite.2.5 90.0 high154.01 335.0ZVQ Quartz vein with minor chalcopyrite and pyrite.3 50.0 high155.75 355.0ZVQ Quartz vein with minor chalcopyrite and pyrite.3.5 45.0 high159.70 182.0ZVQ Quartz vein containing significant pyrite, +/- chalcopyrite.3 43.0 high159.94 315.0SCI Dyke contact0.05 65.0 high160.56 315.0SCI Dyke contact0.05 64.0 high162.02 350.0ZVO Gypsum vein.1.3 40.0 high162.87 325.0ZVQ Quartz veinlet with associated pyrite and chalcopyrite.1.5 67.0 high165.34 94.0ZVO Gypsum veinlet.0.2 70.0 high166.06 311.0ZVO Early quartz veinlet with associated sulphides.1 62.0 high168.67 319.0ZVQ Early quartz vein with associated sulphides.2.5 70.0 high171.18 172.0ZVQ Narrow quartz veinlet with significant pyrite/chalcopyrite.0.8 70.0 high186.16 300.0ZVE Epidote veinlet. May be part of a set.0.2 68.0 high191.33 235.0ZVO Magnetite-chalcopyrite-pyrite vein. Appears to be an isolated occurrence.0.7 30.0 high191.71 285.0ZVQ Quatrz vein with abundant pyrite and Chalcopyrite0.3 35.0 high191.94 300.0ZVQ Quartz vein with minor pyrite0.5 78.0 high193.95 305.0ZVQ Quartz vein with lesser Epidote1 43.0 high194.95 282.0ZVQ Barren Quartz vein1.2 61.0 high195.90 315.0ZVQ Quatrz vein with associated epidote and prite0.8 60.0 high196.54 288.0ZVO Magnetite veinlet with minor pyrite0.7 64.0 high201.49 200.0ZVQ Quartz vein with significant pyrite and chalcopyrite1.2 63.0 high212.49 245.0ZVQ Quartz-magnetite vein, banded with pyrite.7 48.0 high229.10 305.0ZVQ Quartz-magnetite veinlet. Local fabric runs parallel.1.4 25.0 high231.60 315.0ZVQ Quartz-feldspar-pyrite veinlet.2 42.0 high236.63 285.0SFS Fabric- aligned chlorite.0.05 28.0 high237.61 70.0ZVQ Thick milky quartz vein with minor pyrite and chalcopyrite.5 53.0 high238.12 90.0SCI Upper contact of large milky quartz vein, +/- pyrite/chalcopyrite.0.05 45.0 high243.57 355.0ZVQ Narrow milky quartz veinlet with large blebs of pyrite.1 20.0 high257.46 285.0ZVQ Quartz vein3.5 34.0 high

SamplesFrom To Sample typeSample ID Cu_ppm Au_ppb Mo_ppm Pb_ppm Zn_ppm As_ppm Ag_ppm Hg_ppm Sb_ppmK_ppm Bi_ppm S_%

9.00 15.00 410052 CORE_HALF 174.9 50 1.87 25.65 300.7 12.6 0.476 0.035 0.452400 0.12 1.97

15.00 18.00 410053 CORE_HALF 229.95 140.3 2.43 33.21 4752.1 11.7 0.653 0.526 0.662200 0.16 3.72

18.00 20.00 410054 CORE_HALF 705.64 317.4 4.58 25.46 10000 18 1.794 3.249 0.862300 0.23 4.44

20.00 22.00 410055 CORE_HALF 335.03 37.8 4.43 24.22 349.5 11.6 0.691 0.037 0.632800 0.17 2.96

22.00 24.00 410056 CORE_HALF 634.83 48.2 6.05 22.12 761 19.1 1.261 0.161 0.552900 0.2 3.12

24.00 26.00 410057 CORE_HALF 1006.23 97.1 5.98 33.06 1029.1 27.4 2.172 0.278 0.722500 0.3 3.1

KL06_30 10 May 2007 Page 8 of 13

26.00 28.00 410058 CORE_HALF 2039.8 103.2 3.47 14.79 584.7 14.8 2.79 0.125 0.572100 0.11 2.19

28.00 30.00 410059 CORE_HALF 818.28 171.4 8.86 15.69 522.8 20.3 2.856 0.117 0.612200 0.23 3.43

30.00 31.00 410060 CORE_HALF 603.02 86.3 6.39 10.48 361.9 19.9 1.623 0.063 0.463000 0.41 2.82

31.00 34.44 410061 CORE_HALF 350.78 59.7 6.64 8.54 331.9 13.9 0.794 0.047 0.252600 0.28 2.5

34.44 36.00 410062 CORE_HALF 292.3 49 2.86 9.68 155.9 12 0.773 0.008 0.283000 0.23 3.03

36.00 38.00 410063 CORE_HALF 635.06 93.7 5.32 14.7 161.9 11 1.528 0.009 0.292500 0.16 3.87

38.00 40.00 410064 CORE_HALF 479.25 66.1 2.65 8.73 305.6 9.7 1.181 0.013 0.272200 0.07 1.49

40.00 42.00 410065 CORE_HALF 239.97 54.2 2.82 6.73 181.8 5.6 1.061 0.008 0.132700 0.1 2.38

42.00 44.00 410066 CORE_HALF 544.43 51.7 3.12 9.55 195.5 9 0.834 0.014 0.22400 0.17 3.35

44.00 46.00 410067 CORE_HALF 525.01 32.4 3.33 11.22 357 7.1 0.769 0.032 0.352100 0.1 2.5

46.00 48.00 410068 CORE_HALF 1271.82 89.9 2.39 5.45 203.2 6.4 1.394 0.01 0.213100 0.13 1.9

48.00 50.00 410069 CORE_HALF 165.09 29 1.99 5.2 127.8 2.7 0.318 0.023 0.162300 0.06 1.07

50.00 52.00 410071 CORE_HALF 1615.58 62.1 2.59 4.05 129.1 4.3 1.444 0.013 0.343900 0.07 1.72

52.00 54.00 410072 CORE_HALF 827.68 26.8 4.23 5.5 206.3 5.9 0.649 0.015 0.323900 0.11 2.35

54.00 56.00 410073 CORE_HALF 1204.54 48.6 3.45 11.86 274.8 7.4 0.969 0.032 0.34100 0.08 2.55

56.00 58.00 410074 CORE_HALF 588.05 27.1 2.53 18.29 298.4 7.4 0.537 0.044 0.273000 0.09 3.12

58.00 60.00 410075 CORE_HALF 268.5 22.3 2.17 16.48 121.4 5.9 0.347 0.014 0.233000 0.08 1.82

60.00 62.00 410076 CORE_HALF 1097.9 41.2 2.16 11.24 217.4 7.5 0.89 0.032 0.274400 0.07 2.42

62.00 64.00 410077 CORE_HALF 775.69 43.3 2.21 10.66 288.8 7.7 0.734 0.042 0.264300 0.07 1.7

64.00 66.00 410078 CORE_HALF 859.8 36.7 3.05 10.14 176.7 7.3 0.682 0.019 0.263700 0.06 2.22

66.00 68.00 410079 CORE_HALF 2441.3 87.5 3.59 11.59 154.9 9.5 1.266 0.034 0.294600 0.1 2.86

68.00 70.00 410080 CORE_HALF 1765.55 62.8 2.67 11.75 254.5 10 1.1 0.047 0.362900 0.08 1.1

70.00 72.00 410081 CORE_HALF 2044.93 68.8 3.86 6.87 183.9 7.1 0.911 0.04 0.282800 0.12 1.52

72.00 74.00 410082 CORE_HALF 3497.42 102.7 3 6.53 122 8.8 1.596 0.038 0.32400 0.14 1.76

74.00 76.00 410083 CORE_HALF 2641.59 85 1.99 4 185.4 4.9 1.294 0.031 0.211800 0.07 1.28

76.00 78.00 410084 CORE_HALF 2134.48 76.2 0.6 7.82 101.6 2.5 1.729 0.011 0.161500 0.06 0.56

78.00 80.00 410085 CORE_HALF 379.39 16.9 0.91 6.89 104.5 2.8 0.309 0.011 0.121800 0.06 0.74

80.00 82.00 410086 CORE_HALF 2307.09 93.7 1.45 3.64 171.5 8 1.648 0.009 0.161300 0.1 1.37

82.00 84.00 410087 CORE_HALF 2007.48 104.5 1.48 3.13 163 4.9 1.664 0.021 0.131900 0.06 1.16

84.00 86.00 410088 CORE_HALF 1224.02 70.7 1.44 2.88 127.3 4.1 0.885 -0.005 0.161900 0.04 0.43

86.00 88.00 410089 CORE_HALF 794.46 50.3 1.65 2.22 141.5 2 0.558 -0.005 0.091000 0.04 0.28

88.00 90.00 410091 CORE_HALF 1498.43 80.6 1.02 1.85 86.2 1.9 0.653 0.006 0.081400 0.04 0.35

90.00 92.00 410092 CORE_HALF 745.89 57 1.57 4.8 135 4.4 0.687 0.015 0.751700 0.06 1.13

92.00 94.00 410093 CORE_HALF 2435.25 88 1.56 2.49 193.1 4.1 1.217 0.01 0.161200 0.05 0.82

94.00 96.00 410094 CORE_HALF 1399.4 70 1.32 1.36 87.9 2.5 0.768 -0.005 0.11400 0.03 0.39

96.00 98.00 410095 CORE_HALF 845.95 45.3 1.1 1.92 102.6 3.6 0.526 0.005 0.191100 0.03 0.27

98.00 100.00 410096 CORE_HALF 1306.54 78.7 1.56 1.53 99.4 3.2 1.035 0.007 0.091300 0.05 1.41

KL06_30 10 May 2007 Page 9 of 13

100.00 102.00 410097 CORE_HALF 615.01 56.4 1.43 3.59 92.3 5.1 0.989 0.011 0.11200 0.07 3.74

102.00 104.00 410098 CORE_HALF 1823.25 152.1 1.6 6.19 76 1.8 2.009 0.012 0.121200 0.07 3.93

104.00 106.00 410099 CORE_HALF 727.89 54 1.54 2.62 131.3 0.7 0.825 -0.005 0.07600 0.03 2.94

106.00 108.00 410100 CORE_HALF 1144.31 107.4 3.6 3.52 200 1.2 0.705 0.018 0.131000 0.25 3.44

108.00 110.00 410101 CORE_HALF 1924.67 206.6 1.98 3.15 131.1 1.3 1.064 0.009 0.141100 0.16 3.94

110.00 112.00 410102 CORE_HALF 1969.26 271.9 1.39 1.76 102.2 2.4 1.141 0.022 0.131100 0.15 3.61

112.00 114.00 410103 CORE_HALF 1731.49 182 2.02 2.04 83.2 2.7 0.824 0.018 0.111100 0.22 3.91

114.00 116.00 410104 CORE_HALF 4116.72 1427.2 1.2 2.74 71.1 1.1 1.542 0.021 0.141400 0.57 3.03

116.00 118.00 410105 CORE_HALF 4115.09 875.7 1.71 58.5 52.4 1.4 1.358 0.016 0.13900 0.17 3.03

118.00 120.00 410106 CORE_HALF 5760.46 1002.5 1.06 1.64 105.6 0.8 2.13 0.021 2.81500 0.29 2.9

120.00 122.00 410107 CORE_HALF 11290 2940.1 1.5 1.74 58.9 1.3 3.818 0.053 0.13900 0.22 2.62

122.00 124.00 410108 CORE_HALF 4322.19 769.6 3.42 1.29 35.4 1.1 1.039 0.016 0.13700 0.16 2.8

124.00 126.00 410109 CORE_HALF 5506.01 1387.9 2.33 1.55 54.3 1.4 1.685 0.014 0.13700 0.17 2.6

126.00 128.00 410111 CORE_HALF 4580.35 2144.1 1.19 1.42 57.1 0.8 2.443 0.016 0.13600 0.11 2.58

128.00 130.00 410112 CORE_HALF 2690.74 662.8 2.44 1.41 56.7 2.6 1.213 0.017 0.111000 0.26 3.11

130.00 132.00 410113 CORE_HALF 1705.79 318.7 1.2 1.99 81.9 1.7 0.751 0.016 0.1700 0.17 2.36

132.00 133.00 410114 CORE_HALF 10630 2036.6 1.3 3.7 83.9 2 4.228 0.027 0.14500 0.2 2.33

133.00 134.00 410115 CORE_HALF 37740 11198.3 0.71 3.73 94.1 4.2 15.504 0.081 0.3600 0.4 4.4

134.00 135.00 410116 CORE_HALF 29890 8100.5 0.88 3.13 105.8 2.2 10.549 0.057 0.27600 0.36 4.5

135.00 137.00 410117 CORE_HALF 2392.72 323.9 2.05 3.88 111.1 0.9 1.196 0.009 0.07600 0.1 1.54

137.00 139.00 410118 CORE_HALF 5573.85 1363.6 1.39 2.75 75.3 1.7 2.402 0.018 0.16600 0.24 3.15

139.00 141.00 410119 CORE_HALF 6672.86 1443.9 1.61 2.27 100.5 1.7 3.022 0.037 0.12600 0.23 2.74

141.00 143.00 410120 CORE_HALF 2847.1 285 2.17 1.23 36.9 1.4 1.229 0.01 0.111100 0.14 3.78

143.00 145.00 410121 CORE_HALF 2869 648.5 0.75 0.9 44.1 1.4 1.328 0.025 0.11000 0.33 3.64

145.00 147.00 410122 CORE_HALF 2809.15 424.1 0.98 1.06 43.8 0.5 1.221 0.027 0.07600 0.22 2.47

147.00 149.00 410123 CORE_HALF 1509.04 123.1 1.69 0.8 31 0.8 0.587 0.008 0.07700 0.08 4.1

149.00 151.00 410124 CORE_HALF 4680.23 429.3 1.31 0.78 36.5 0.7 1.647 0.015 0.121000 0.41 4.94

151.00 153.00 410125 CORE_HALF 3773.91 315.4 5.36 0.86 41.9 0.9 1.306 0.024 0.091100 0.14 2.82

153.00 155.00 410126 CORE_HALF 2665.36 128.1 1.44 0.92 48.9 1 0.847 0.017 0.071000 0.1 3.75

155.00 157.00 410127 CORE_HALF 2714.72 316.8 1.3 0.57 29.4 0.9 1.092 0.012 0.061000 0.18 4.48

157.00 159.00 410128 CORE_HALF 3935.52 211.1 1.21 0.9 39.5 1.2 1.043 0.026 0.061000 0.19 3.74

159.00 161.00 410129 CORE_HALF 3230.45 125.1 1.83 0.93 60.9 1.2 0.929 0.028 0.08700 0.1 3.09

161.00 163.00 410131 CORE_HALF 2571.71 134.6 1.04 0.77 44.3 1.5 0.798 0.021 0.051100 0.13 3.43

163.00 165.00 410132 CORE_HALF 1689.9 59.9 0.99 1.92 54.1 1.2 0.763 0.023 0.061000 0.05 3.32

165.00 167.00 410133 CORE_HALF 2078.86 65.8 1.67 0.65 39.6 1.3 0.562 0.007 0.05900 0.09 3.5

167.00 168.00 410134 CORE_HALF 2622.89 101.5 2.39 0.72 56.8 2 1.105 0.017 0.08900 0.17 3.68

168.00 169.00 410135 CORE_HALF 2253.6 272.3 6.33 0.8 27.1 1 0.634 0.01 0.04700 0.06 3.95

KL06_30 10 May 2007 Page 10 of 13

169.00 170.00 410136 CORE_HALF 5226.6 268.1 19.1 0.61 33.2 1.2 0.911 0.023 0.06500 0.09 3.11

170.00 172.00 410137 CORE_HALF 1882.94 69.9 13.31 1.1 56.1 1.2 0.619 0.018 0.09500 0.05 3.01

172.00 174.00 410138 CORE_HALF 851.52 54.4 2.42 0.73 53.9 1.8 0.354 0.007 0.08800 0.08 2.66

174.00 175.50 410139 CORE_HALF 51.36 33.2 0.88 6.18 56 2.5 0.264 0.05 0.221500 0.04 0.46

175.50 177.00 410140 CORE_HALF 1081.7 78.5 4.25 0.97 41.9 1.6 0.695 -0.005 0.051100 0.15 4.97

177.00 179.00 410141 CORE_HALF 1461.34 103 4.09 0.78 35.4 1.6 0.738 -0.005 0.051400 0.09 4.1

179.00 181.00 410142 CORE_HALF 2876.23 234.9 4.61 0.56 40.6 1.3 1.296 0.012 0.071200 0.15 3.91

181.00 183.00 410143 CORE_HALF 2234.97 262.7 1.06 0.46 49.4 1.1 1.012 0.007 0.141100 0.11 3.28

183.00 185.00 410144 CORE_HALF 706.68 118.6 1.2 0.91 51.3 0.9 0.34 0.013 0.111200 0.12 2.68

185.00 187.00 410145 CORE_HALF 1584.47 263.9 0.89 1.16 55.4 2 0.663 0.019 0.261000 0.16 3.08

187.00 189.00 410146 CORE_HALF 608.01 115.8 0.65 0.52 48.5 0.8 0.251 0.01 0.121100 0.08 2.55

189.00 191.00 410147 CORE_HALF 2261.89 253.2 1.13 0.65 56 1 0.946 0.018 0.05900 0.13 2.08

191.00 193.00 410148 CORE_HALF 1841.35 365 1 0.57 53.4 1.9 0.599 0.018 0.061200 0.19 2.54

193.00 195.00 410149 CORE_HALF 381.69 103.1 1.05 0.58 55.4 1.8 0.194 0.01 0.161300 0.28 3.03

195.00 197.00 410151 CORE_HALF 856.42 141.8 0.77 0.57 46 1.9 0.46 0.007 0.051200 0.15 4.5

197.00 199.00 410152 CORE_HALF 554.86 136.9 0.73 0.61 37.5 2 0.402 0.016 0.051300 0.33 3.49

199.00 201.00 410153 CORE_HALF 1863.36 315 0.94 0.7 54.1 2.1 1.073 0.018 0.061000 0.06 3.15

201.00 203.00 410154 CORE_HALF 1900.59 356.3 1.15 0.82 56.8 2.5 0.917 0.024 0.071000 0.09 2.3

203.00 205.00 410155 CORE_HALF 1325.69 162.5 1.38 1.27 50 0.7 0.646 0.017 0.06900 0.06 2.56

205.00 207.00 410156 CORE_HALF 2547.37 1693.6 6.37 1.62 47.9 0.9 1.907 0.032 0.08800 0.34 3.61

207.00 209.00 410157 CORE_HALF 2644.31 347.8 0.72 1.34 78.9 1.2 1 0.01 0.12900 0.1 1.61

209.00 211.00 410158 CORE_HALF 2030.19 361.5 0.84 1.92 80.6 2 0.821 0.008 0.12800 0.12 2.02

211.00 212.00 410159 CORE_HALF 2980.56 598.7 7.6 2.51 63.7 2.6 3.197 0.014 0.121000 0.23 2.75

212.00 213.00 410160 CORE_HALF 1465.78 432.8 1.14 2.06 58.4 4.1 1.073 0.006 0.11000 0.42 2.47

213.00 214.00 410161 CORE_HALF 1905.4 458.9 93.07 1.68 58.2 0.7 1.044 0.005 0.081000 0.14 1.12

214.00 216.00 410162 CORE_HALF 1691.73 472.5 3.39 1.72 48.9 0.5 1.948 0.006 0.12900 0.2 1.56

216.00 218.00 410163 CORE_HALF 984.85 827.4 7.03 1.9 84.4 0.6 3.32 0.005 0.132800 0.34 1.93

218.00 220.00 410164 CORE_HALF 1309.36 159.6 129.03 1.26 105.8 0.3 1.303 0.007 0.081000 0.15 1.39

220.00 222.00 410165 CORE_HALF 2504.41 513.5 40.49 1.68 110.1 1.1 2.669 0.008 0.131200 0.25 1.86

222.00 223.00 410166 CORE_HALF 2650.09 894.7 1.43 1.37 97.3 0.7 3.206 -0.005 0.12700 0.25 1.69

223.00 224.00 410167 CORE_HALF 721.76 4719.2 2.86 5.31 40.8 3.4 20.825 0.048 0.22100 1.64 5.35

224.00 225.20 410168 CORE_HALF 63.61 3216.4 4.79 1.64 7.7 3 12.879 0.025 0.131300 0.64 3.65

225.20 227.00 410169 CORE_HALF 740.5 683.8 2.05 3.7 31.3 2.1 3.629 -0.005 0.182300 0.58 4.14

227.00 228.00 410171 CORE_HALF 1017.22 804.3 116.32 2.72 48.5 0.6 3.732 0.007 0.081500 0.42 3.79

228.00 229.00 410172 CORE_HALF 1071.08 342.6 48.12 2.43 61.1 0.3 1.921 -0.005 0.171200 0.3 3.17

229.00 230.00 410173 CORE_HALF 2107.66 656 1.58 1.76 60.2 1.7 3.276 -0.005 0.141300 0.49 2.62

230.00 231.00 410174 CORE_HALF 1084.32 150.7 0.67 1.47 54.1 0.2 1.119 -0.005 0.111300 0.09 1.6

KL06_30 10 May 2007 Page 11 of 13

231.00 232.00 410175 CORE_HALF 2334.18 329 0.82 2.5 46.6 0.9 2.173 0.006 0.181600 0.28 3.8

232.00 234.00 410176 CORE_HALF 1339.9 240.5 3.19 1.93 57.6 0.2 1.333 -0.005 0.161400 0.2 2.43

234.00 236.00 410177 CORE_HALF 1734.54 289.9 1.5 1.82 48.4 -0.1 1.776 -0.005 0.151700 0.18 2.41

236.00 237.00 410178 CORE_HALF 2528.55 409 3.99 1.76 30.5 0.3 2.295 -0.005 0.151700 0.19 2.79

237.00 238.30 410179 CORE_HALF 679.09 1066 11.2 3.25 65.4 1.4 4.413 0.007 0.151400 0.76 4.94

238.30 239.80 410180 CORE_HALF 1085.86 10740.7 2.7 0.99 3 0.5 42.134 0.037 0.09500 2.22 1.31

239.80 241.00 410181 CORE_HALF 411.73 218.4 7.11 2.17 18.1 1.6 1.377 -0.005 0.152000 0.35 2.83

241.00 243.00 410182 CORE_HALF 257.4 253.9 3.08 2.2 22.9 0.9 1.663 -0.005 0.12200 0.27 1.88

243.00 245.00 410183 CORE_HALF 282.89 190.2 2.64 2.18 20.8 1.6 1.818 -0.005 0.132000 0.27 2.92

245.00 247.00 410184 CORE_HALF 361.84 219.2 1.28 1.97 38.6 0.5 1.613 0.018 0.152200 0.18 2.51

247.00 248.00 410185 CORE_HALF 362.61 268.2 0.76 3.47 63.3 0.8 2.106 0.012 0.22000 1.11 5.45

248.00 249.10 410186 CORE_HALF 456.9 438.4 6.55 6.08 66.8 3.8 3.033 0.01 1.421700 2.34 6.07

249.10 251.00 410187 CORE_HALF 380.78 207.4 0.88 2.85 26.1 0.6 0.831 0.021 0.112300 0.38 4.06

251.00 253.00 410188 CORE_HALF 509.1 185.5 1 2.08 28.8 0.6 0.609 0.009 0.142000 0.19 1.95

253.00 255.00 410189 CORE_HALF 650.52 158.3 0.87 1.27 50 0.9 0.503 -0.005 0.11500 0.09 1.02

255.00 257.00 410191 CORE_HALF 524.64 309.9 1.09 1.75 54.8 0.5 0.476 0.008 0.071700 0.2 1.69

257.00 259.00 410192 CORE_HALF 515.21 173.4 17.21 1.25 44.9 1.2 0.585 -0.005 0.061000 0.28 2.38

259.00 261.00 410193 CORE_HALF 200.55 40.9 6.88 0.91 44.4 0.8 0.16 -0.005 0.041000 0.11 1.39

261.00 263.00 410194 CORE_HALF 288.65 42.5 11.63 0.91 36.6 1.1 0.237 -0.005 0.06900 0.13 1.5

263.00 265.00 410195 CORE_HALF 458.55 62.8 15.43 0.85 39.4 0.7 0.375 -0.005 0.071100 0.07 1.34

265.00 267.00 410196 CORE_HALF 34.27 23.7 0.4 0.61 74 0.5 0.031 -0.005 0.081900 -0.02 0.1

267.00 269.00 410197 CORE_HALF 126.55 276.7 0.64 0.84 319.8 0.8 0.152 0.015 0.082000 -0.02 0.14

269.00 271.00 410198 CORE_HALF 52.67 40.2 0.55 0.85 111.6 0.6 0.05 -0.005 0.12100 -0.02 0.13

271.00 273.00 410199 CORE_HALF 362.44 133.6 15.19 0.81 46 0.6 0.306 -0.005 0.051000 0.06 2.1

273.00 275.00 410200 CORE_HALF 290.26 59.9 0.69 0.69 45.1 1 0.203 -0.005 0.051900 0.02 0.94

275.00 277.00 410201 CORE_HALF 1505.58 309.9 38.92 0.66 40.3 1 0.929 -0.005 0.091200 0.2 2.1

277.00 279.00 410202 CORE_HALF 1189.27 352.7 0.77 0.91 40.2 2.3 0.753 -0.005 0.08700 0.23 1.24

279.00 281.00 410203 CORE_HALF 817.82 123.8 0.71 0.79 62.9 0.9 0.381 -0.005 0.08700 0.05 0.35

281.00 283.00 410204 CORE_HALF 960.28 213.9 1.03 0.47 81.9 1.4 0.566 -0.005 0.07800 0.06 0.58

283.00 285.00 410205 CORE_HALF 765.96 174.9 1.26 0.55 74.1 1.7 0.403 -0.005 0.061100 0.04 0.63

285.00 287.00 410206 CORE_HALF 1174.76 175.4 3.15 0.7 62.2 0.4 0.673 -0.005 0.06800 0.03 0.69

287.00 289.00 410207 CORE_HALF 639.43 162.8 0.62 0.36 53.3 0.8 0.383 -0.005 0.05800 0.03 0.92

289.00 291.00 410208 CORE_HALF 680.86 140.9 0.82 0.54 64.9 0.7 0.432 -0.005 0.05800 0.02 0.62

291.00 293.00 410209 CORE_HALF 536.47 153.6 0.33 0.6 62.3 0.5 0.317 -0.005 0.08800 0.02 0.28

293.00 295.00 410211 CORE_HALF 672.34 193.8 0.62 1.01 55.6 0.7 0.499 0.007 0.08800 0.07 1.32

295.00 297.00 410212 CORE_HALF 703.46 156.9 0.73 0.98 68 1.1 0.428 -0.005 0.09500 0.08 0.59

297.00 299.00 410213 CORE_HALF 582.03 237.8 0.53 0.87 79.2 1 0.257 -0.005 0.08300 0.04 0.39

KL06_30 10 May 2007 Page 12 of 13

299.00 301.00 410214 CORE_HALF 449.1 117.8 0.27 0.88 99.1 0.4 0.327 -0.005 0.08400 0.04 0.4

301.00 303.00 410215 CORE_HALF 501.97 95.8 0.95 1.83 71.6 0.4 0.348 -0.005 0.051200 0.05 0.44

303.00 305.00 410216 CORE_HALF 861.73 160.2 0.66 1.52 80.2 0.5 0.535 -0.005 0.05800 0.07 0.31

305.00 307.00 410217 CORE_HALF 1205.78 283.5 0.63 1.97 74.6 4.9 0.789 -0.005 0.11800 0.39 2.09

307.00 309.00 410218 CORE_HALF 978.62 205.5 0.51 1.54 93.9 2.3 0.554 -0.005 0.1500 0.16 1.56

309.00 311.00 410219 CORE_HALF 576.93 152.7 0.28 1.14 72.1 0.4 0.31 -0.005 0.08400 0.04 0.45

311.00 313.00 410220 CORE_HALF 501.85 80.6 1.5 1 57.9 0.6 0.294 -0.005 0.1400 0.04 1.02

313.00 315.00 410221 CORE_HALF 263.14 43.2 0.99 1.28 39.8 1 0.156 -0.005 0.06600 0.04 0.6

315.00 317.00 410222 CORE_HALF 911.17 102.9 1.43 1.13 40.8 0.7 0.531 -0.005 0.07600 0.07 0.83

317.00 319.00 410223 CORE_HALF 625.59 175.1 2.06 4.22 46.7 1.2 0.919 -0.005 0.131000 0.08 2.01

319.00 321.00 410224 CORE_HALF 1223.84 299.4 1.47 2.09 35.9 1.5 0.803 -0.005 0.09700 0.09 1.42

321.00 323.00 410225 CORE_HALF 2864.79 802.5 0.7 1.7 47.8 4.2 1.499 0.005 0.16800 0.38 2.59

323.00 325.37 410226 CORE_HALF 3305.06 1724.4 1 2.82 50.9 7.5 1.798 -0.005 0.16400 0.52 2.1

KL06_30 10 May 2007 Page 13 of 13

KL06_31GEOINFORMATICS EXPLORATIONDRILL HOLE LOG

Geoinformatics Exploration Inc

KL06_31

Kliyul

426.11

NAD83_UTM_09

6265954.00

1775.00 mGXL_KLIYUL_2006

DDHole ID

DataSet

Prospect

Hole type

Depth

Notes

Collar

m

30/08/2006Commenced

05/09/2006Completed

Drilling company

Tenement

Grid ID

Geologist

Survey Method

Easting

Northing

676520.00 RL

At Dip MethodAzimuth AzimuthID CommentsSurvey

41.45 -71.4224.6 CAMERANAD83_UTMm102.41 -71.6218.7 CAMERANAD83_UTMm163.37 -71.1207.9 CAMERANAD83_UTMm224.33 -71.1216.7 CAMERANAD83_UTMm285.29 -71.2208.0 CAMERANAD83_UTMm346.25 -71.1201.4 CAMERANAD83_UTMm407.21 -71.0219.8 CAMERANAD83_UTMm

LithologyFrom To Code GSize Text1 %

Logged by: Mclean_Trottm CommentsText2Qual Code GSize Text1 %Text2Qual

Lith 1 Lith 2

0.00 13.72 CASE 100

13.72 70.26 XSH F fo 100eqcl

70.26 73.90 VIOP C pp 100cl

73.90 90.28 XSH F fo 100eqcl

90.28 97.12 VIO M cr 100cl

97.12 99.26 VIB F cr 100eqcl

99.26 170.55 XSH F fo 100cl

170.55 171.32 III M cr 100eqcl

171.32 180.05 XSH F fo 100cl

180.05 205.04 IIO M cr 100cl

205.04 224.66 VIO F cr 100cl

224.66 238.83 XSH F fo 100cl

KL06_31 10 May 2007 Page 1 of 14

238.83 293.88 VIO F cr 100cl

293.88 335.40 XSH F cr 100cl

335.40 346.91 III M cr 100eqcl

346.91 374.78 IIO M cr 100cl

374.78 391.56 IIP F pp 100cl

391.56 426.11 VIO F cr 100cl

LithologyFrom To

Logged by: Mclean_Trottm Description

0.00 13.72

13.72 70.26 Chloritic schist- Interval is extremely chloritic, schistose rock, generally very crumbly and non-cohesive. Chloritization has obliterated primary textures/structures to the extent whdetermination of protolith becomes problematic, however, this interval is likely dominated by volcanic/volcaniclastic intermediate rocks (altered andesites). For the purposes of thlog, rocks of this nature, wherein relict textures/structures are not observed will be classified as chloritic schists, regardless of the actual schistosity of the rock (degree of developof schistosity will be noted). Where relict features are observed, an attempt will be made to classify the lithology based on protolith, as "chloritic schist" is rather generic.

70.26 73.90 Plagioclase-porphyritic intermediate volcanics- Interval is also highly chloritized- however, relict plagioclase phenocrysts may still be observed (although corroded).

73.90 90.28 Chloritic schist- Interval is extremely chloritic, schistose rock, generally very crumbly and non-cohesive. Chloritization has obliterated primary textures/structures to the extent whdetermination of protolith becomes problematic, however, this interval is likely dominated by volcanic/volcaniclastic intermediate rocks (altered andesites).

90.28 97.12 Intermediate volcanic rock- Interval is strongly chloritized. Grain size appears to be significantly larger than the overlying schist, although grain boundaries are indistinct. Two possibilities for protolith exist for this rock: fine-grained, shallow-level intrusive intermediate rock, or porphyritic intermediate volcanic rock. Relict textures are subtle, but suggestplagioclase-porphyritic volcanic rock. This conclusion, however, is far from definitive and may be subject to interpretation. Lower portion of the interval grades back into chloritic with a well-developed fabric.

97.12 99.26 Basaltic andesite- Rock is dark olive green, darker than surrounding schist, and displays weak to nonexistent fabric. Fine-grained, equigranular rock with relatively commonplaccalcite veining.

99.26 170.55 Chloritic schist- Interval has been strongly chloritized, obliterating primary textures/structures. A moderately developed fabric is ubiquitous, although subtle in some portions, espwhere protolith resembles the "basaltic andesite" described above. Local areas of sericitic overprint- greyish white rock as opposed to pale blue-green chloritic material. Possiblpegmatite dykelet observed from 152.61 to 152.97 m depth. This feature is pre-metamorphic, and consists of large, irregular masses of k-feldspar and quartz, with subordinate plagioclase.

170.55 171.32 Monzodiorite- Interval has a relict igneous texture. Appears to be pre-metamorphic, although less affected by the metamorphism than adjacent volcaniclastics (chloritic schist). Iis pale greenish-white, dominated by felsic minerals with evenly distributed flecks of chlorite throughout (retrograded from hornblende?). Monzodiorite is a tentative classification

171.32 180.05 Chloritic schist- As described previously. Possible relict plag-phyric textures observed, suggestive of porphyritic andesite flows as protolith.

180.05 205.04 Intermediate intrusive rock (diorite?)- Similar to overlying chloritic schist, however, is less chloritized and possesses a weak to nonexistent fabric (more resistant to metamorphisRelict igneous textures seen commonly. Local areas of more intense alteration.

205.04 224.66 Intermediate volcanic rock- Interval is aggressively chloritized. A subtle fabric is present locally, created by alignment of relict plagioclase phenocrysts (flow alignment?). Rock igenerally fine-grained, with very subtle relict textures. Protolith is questionable, and may not necessarily be volcanic. An interesting feature of this interval is the abundance of qufragments, containing a strong lineation imparted by banding of fine-grained magnetite. These quartz fragments are truncated and offset extensively. They may represent very equartz veins with rhythmic banding, or possibly be fragments of meta-sandstone, torn up and included by an intermediate volcanic flow. The first hypothesis is most likely (early qveins).

224.66 238.83 Chloritic schist- An extremely heterogeneous interval, with well-developed fabric throughout (locally intense). Rocks are dominantly chloritic, although sericitic overprint is observcommonly.

238.83 293.88 Intermediate volcanic rock (?)- Strongly chloritic, with weak to absent fabric. Protolith is questionable, due to lack of relict textures/structures. Local zones of pale, sericitic (QSPmaterial. Occasional subtle fabric.

293.88 335.40 Chloritic schist- Rock is chloritic. Schistosity is weak to nonexistent although the rock is classified as such to indicate that protolith is very much indeterminate (little or no relict textures/structures preserved). Fine grained nature of interval suggests a volcanic/volcaniclastic origin, although this conclusion is not definitive. Epidote fracture veining relativecommonplace. Sericite notably absent.

KL06_31 10 May 2007 Page 2 of 14

AlterationFrom To Alt1 Style Int.m CommentsAlt2 Style Int. Alt3 Style Int.Total Int.

13.72 44.95 CH pv STG Dominant alteration style in this interval is pervasive chlorite- protolith has been extensivchloritized. Lesser amounts of calcite are present, as fracture fill/veinlets.

CN ff WKSTG

44.95 48.75 CH pv STG Alteration in this interval is similar to the overlying interval; however, epidote is now present, coating fractures. Calcite is still present as fracture-fill, but also locally disseminated through the rock.

EZ fsel MOD CN ff WKSTG

48.75 69.22 CH pv STG Alteration seen is similar to overlying alteration. Protolith has been pervasively chloritizeEpidote is generally absent in this interval, except in rare fractures. Calcite is rare to absent. Narrow, localized patches of pale, greyish-white sericitic-altered material prese

SR pv WKSTG

69.22 69.80 SR pv STG Pervasive chloritic alteration has been overprinted by pervasive sericite. Interval has a greyish-white hue.

CH pv WKSTG

69.80 73.90 CH pv MOD Interval appears to be altered to a lesser extent than the overlying rock. Relict textures preserved somewhat. Carbonate (calcite) is commonplace, disseminated throughout, possibly replacing plagioclase phenocrysts.

CN diss WKMOD

73.90 90.28 CH pv STG Protolith has been pervasively chloritized. Epidote is generally absent in this interval. Calcite is rare, seen locally as veinlets. Narrow, localized patches of pale, greyish-whitesericitic-altered material present (overprint).

SR pv WK CN ff TRSTG

90.28 97.12 CH pv MOD Interval appears to be altered to a lesser extent. Relict textures are preserved somewhaCarbonate (calcite) is observed, disseminated throughout the upper portion of the interv

CN diss TRMOD

97.12 99.26 CN vsel MOD Interval is relatively weakly altered. Chloritization has progressed to a lesser extent. Fabric is weak to nonexistent. The most definitive alteration observed is wispy, irregularcalcite veinlets. Interval is weakly magnetic (disseminated magnetite).

CH pv WK MT diss WKMOD

99.26 102.01 SR pv STG Interval is dominated by pale greyish-white sericitic material with accessory pyrite (phyllialteration? QSP?) overprinting chloritic alteration. Chloritic alteration is locally preservedMinor carbonate present.

CH pv MOD CN vsel WKSTG

102.01 104.97 CH pv STG Interval is characterized by small amounts of epidote veinlets, and by the appearance ofsmall amounts of gypsum veinlets.

EZ vsel WK GP vsel TRSTG

104.97 108.00 CN vsel MOD Calcite veinlets are most characteristic of this interval.CH pv MODSTG108.00 112.55 CH pv STG Interval is characterized by small amounts of epidote veinlets, and by the appearance of

small amounts of magnetite veinlets.EZ vsel WK MT vsel TRSTG

112.55 122.33 CH pv STG Interval contains both gypsum and magnetite veinlets.GP vsel WK MT vsel WKSTG122.33 123.58 SR pv STG Sericite-overprinted interval. Residual chlorite seen locally. The lower half of the interva

is distinctly different, featuring an unusual texture, possibly resulting from deformation ofcoarse grained intrusive.

CH pv WKSTG

123.58 148.35 CH pv STG Interval contains both gypsum and magnetite veinlets in low concentrations. Strongly chloritized rock, moderate to well developed fabric.

GP vsel WK MT vsel WKSTG

148.35 152.61 SR pv STG Similar alteration to overlying interval, except sericitically overprinted to varying degreesCH pv MODSTG152.61 177.00 CH pv STG Dominant alteration style in this interval is pervasive chlorite- protolith has been extensiv

chloritized. Lesser amounts of calcite and gypsum are present, as fracture fill/veinlets.GP vsel WKSTG

177.00 178.03 CH pv STG Interval characterized by thick veins of gypsum.GP vsel STGSTG

335.40 346.91 Monzodiorite- Interval has a relict igneous texture. Appears to be pre-metamorphic, although less affected by the metamorphism than adjacent volcaniclastics (chloritic schist). Iis pale greenish-white, dominated by felsic minerals with evenly distributed euhedral hornblende crystals throughout, generally retrograded almost completely to chlorite. Monzoda tentative classification.

346.91 374.78 Intermediate intrusive rock (diorite?)- Altered to a greater extent than overlying monzodiorite. Relict igneous textures seen commonly. Fabric is weak to nonexistent.

374.78 391.56 Porphyritic intermediate intrusive- Interval is weakly altered, preserving clear-cut relict textures. Strongly plagioclase porphyritic, although locally the plagioclase phenocrysts havaltered entirely to epidote. Porphyritic texture becomes more subtle towards the lower contact of the interval, with phenocrysts becoming hazy, rounded.

391.56 426.11 Intermediate volcanic rocks- Heterogeneous interval, likely dominated by volcanic rocks but containing possible intermediate intrusive rocks as well. Local zones of sericitically overprinted material (QSP).

KL06_31 10 May 2007 Page 3 of 14

178.03 195.60 CH pv MOD Chloritization in this interval appears less extensive than in overlying rock.CN vsel WK MT vsel TRMOD195.60 197.30 SR pv STG Interval is sericitized pervasively, centred on several irregular veins containing quartz,

calcite, and brownish-pink gypsum.GP vsel STG CN vsel MODSTG

197.30 201.20 CH pv STG Pervasively chloritic interval. Thick magnetite veins present.MT vsel MODSTG201.20 209.10 SR pv MOD Interval of pervasive chlorite overprinted irregularly by sericitic alteration (phyllic).CH pv MODSTG209.10 224.66 CH pv STG Strongly chloritized rock. Weak to nonexistent fabric. Magnetite present. MT vsel WKSTG224.66 238.83 SR pv STG Highly altered sequence of rocks, featuring pervasive chlorite with common sericitic

overprint. Chlorite locally has a different hue, almost aquamarine in colour (fuchsite?-- chromium).

CH pv STGSTG

238.83 247.83 CH pv MOD Pervasive chlorite- somewhat weaker than overlying interval. Other types of alteration seen locally.

MOD

247.83 253.44 SR pv STG Pale tan to greyish-white sericitically overprinted rock. Little pyrite present. Magnetite absent (magnetite-destructive alteration). Rare, local gypsum veinlets.

STG

253.44 277.33 CH pv STG Pervasively chloritized interval. Common calcitic microfractures. Local patches of seric(QSP) material.

CN fsel WK SR pv TRSTG

277.33 279.65 SR pv STG Sericitic (QSP) zone. Hosts best copper mineralization seen in this drillhole, in the formwhat appears to be early quartz, and as remobilizations in late gypsum.

GP vsel MODSTG

279.65 335.40 CH pv MOD Interval is pervasively chloritized. Thin, anastomozing epidote veinlets are ubiquitous, although variable. Carbonate microveining common. Local gypsum.

EZ vsel MOD CN vsel WKSTG

335.40 346.91 CH rep MOD Unit altered to a lesser degree (less reactive primary lithology). Primary mafic minerals (hornblende) have been reacted to chlorite, although crystallographically preserved. Mincarbonate microfractures.

CN fsel WKMOD

346.91 374.78 CH pv STG Higher degree of alteration. Pervasive chloritization, accompanied by common calcitic microfractures (+/- quartz), as well as epidote veinlets. Local, restricted intersections of sericitic material containing abundant disseminated pyrite (QSP assemblage).

CN fsel MOD EZ vsel WKSTG

374.78 391.56 EZ rep MOD Most significant alteration style observed is epidote replacement of plagioclase phenocrysts.

CH pv TR CN fsel WKMOD

391.56 407.60 CH pv MOD Small amounts of epidote veining. Local quartz-sericite-pyrite-altered zones (QSP).EZ vsel WK SR pv WKMOD407.60 411.38 SR pv STG Strongly sericitized rock. Associated disseminated pyrite. (QSP).STG411.38 422.93 CH pv MOD Interval of variable alteration. Dominantly chloritic. Epidote veining seen towards the

bottom of the interval. Common calcitic microfracturesSR pv WK EZ vsel TRSTG

422.93 426.11 SR pv STG Sericitic (QSP) interval. STG

VeiningFrom To Vein1 Style Int.m Av. thick



(mm)Av.

AngleAv.

AngleAv.

AngleComments

13.72 90.28 ZVC FRV 2 0.4 2 Interval is dominated by calcite veinlets. Other vein types may be present in lesser amounts, but are difficult to detect due to the rubbly nature of the core.

90.28 104.97 ZVO FRV 3 0.6 ZVC FRV 3 0.4 ZVO 1 0.4 Interval is characterized by the appearance of late gypsum +/- calcite veining. Local magnetite veinlets. Early pyrite veinlets observed. Minor epidote veinletspresent in lower portion of interval (captured as alteration).

104.97 106.32 ZVC WSP 5 0.5 5 Relatively high density of calcite veinlets seen. Little or no other vein types observed.

KL06_31 10 May 2007 Page 4 of 14

106.32 177.05 ZVC FRV 2 0.3 ZVE WSP 2 0.15 ZVO FRV 2 0.35 Variably veined interval. Various combinations/permutations and densities of calcite, gypsum, epidote, and magnetite veins seen. Narrow veinlets/dykelets of what appears to be intergrowths oquartz and plagioclase are commonplace, especially toward the bottom of the interval (magmatic?).

177.05 178.03 ZVO FRV 20 4 2015 Small interval dominated by thick gypsum veins at a shallow angle to the core axis. Late.

178.03 195.60 ZVC FRV 3 0.3 ZVE WSP 3 0.2 ZVO Weakly veined interval. Most common vein type is calcite.

195.60 197.30 ZVO FRV 17 6 17 Interval is characterized by thick, irregular veins of gypsum, calcite, and quartz. Multiple vein phases along the same pathway? Gypsum is unusually brownish-red, rather than the usual greyish-white, semitransparent version (iron content?).

197.30 277.33 ZVQ FRV 2.5 1.5 ZVO FRV 2.5 0.8 ZVC 1.5 0.2 Variably veined interval. Most dominant vein type is quartz with lesser plagioclase +/- pyrite +/- chalcopyrite. These may, however, be magmatic rather than hydrothermal in nature. These veins are seen in a wide range of orientations and thicknesses.Also observed commonly are gypsum veinlets and calcite veinlets. There may be two phases of gypsumpresent- a late, semitransparent phase which seemsto crosscut virtually everything, and an earlier, brownish-pink phase associated with quartz and calcite (timing difficult to assess on this phase). Abundant early quartz-magnetite veining.

277.33 279.65 ZVO FRV 8 3 ZVQ FRV 8 1.2 Strongly veined interval, dominated by late gypsum, locally hosting pyrite and chalcopyrite (remobilizate). Early quartz veins observed.

279.65 335.40 ZVE WSP 2 0.2 ZVQ FRV 2 0.8 ZVC 0.5 0.3 Most distinctive vein type observed in this interval is anastomozing, wispy epidote veinlets with local pyriteand/or chalcopyrite. Other vein types present to a lesser extent include: Early quartz-magnetite veins, calcitic fracture veinlets, and rare gypsum veinlets. Epidote veining appears to be rather late.

335.40 346.91 ZVC FRV 0.8 0.2 0.8 Little veining present. Thin carbonate fracture veinletpresent.

346.91 374.78 ZVE WSP 1 0.25 ZVQ FRV 1 0.8 ZVC WSP 0.7 0.15 Greater abundance and more variety of veining seen.Magnetite and quartz-magnetite veining appears to bearly, followed by variations of epidote veining. Carbonate veining appears to be late (?). Rare, locallate gypsum veining.

374.78 426.11 ZVC WSP 2 0.1 ZVE WSP 2 0.2 ZVQ FRV 1.5 0.8 Variably veined interval. Local intervals feature epidote veining.

KL06_31 10 May 2007 Page 5 of 14

Mineralisation PercentFrom To CCP

Frac CCP Vein

PYDiss

PYFrac

PYOXFrac

PYVein

MAL Frac

CCP Diss

Description

13.72 70.26 0.05 0.8 Interval is strongly pyritized. Little or no chalcopyrite observed. Strongest pyrite mineralization seems tcoincide with more rubbled drillcore. Possible fine-grained galena observed at 19.7 m.

70.26 73.90 Weakly mineralized to nonmineralized interval. Core is more structurally intact than surrounding core aswell.

73.90 90.28 0.05 0.8 Interval is strongly pyritized. Little or no chalcopyrite observed. Strongest pyrite mineralization seems tcoincide with more rubbled drillcore.

90.28 97.12 0.6 Interval of relatively intact core which is strongly pyrite mineralized, in the form of early pyritic veins and pyrite disseminations. Little or no chalcopyrite observed.

99.26 102.01 0.5 Moderately mineralized sericitic interval. Disseminated, fine-grained pyrite dominates. Lesser vein-hospyrite, seen mainly in early quartz veinlets (very deformed, commonly truncated and cross-cut).

102.01 104.14 0.2 Dominant mineralization is vein-style pyrite, hosted mainly by early quartz veins. No chalcopyrite observ108.00 112.55 0.2 Pyrite mineralization hosted mainly by thin, anastomozing, early epidote veinlets (crosscut by calcite

veining).112.55 114.12 0.2 Weakly mineralized zone.114.12 117.60 0.2 Well mineralized interval. Significant chalcopyrite observed. The bulk of mineralization in this interval is

vein-hosted, generally in the form of early quartz veins, occasionally with associated magnetite.117.60 138.15 0.2 Weakly, variably mineralized interval. The bulk of mineralization present is observed in several vein typ

including quartz, quartz-epidote, and magnetite. These veins generally appear to be early.138.15 201.20 0.2 Zone of stronger mineralization. Chalcopyrite is observed, in small quantities. Of possible interest is a

small zone from 143.05 to 143.45 m, consisting of what appears to be deformed quartz and feldspar (eafelsic dyke material?), sheared together with chloritic host rocks, and hosting significant chalcopyrite. Virtually all mineralization observed tends to be centralized in early vein systems. Some minor amountslater mineralization are seen, likely representing sulphides remobilized from pre-existing veinlets, etc. However, the dominant mineralization is early in the post-depositional history of these rocks, and definitpre-metamorphic.

201.20 205.04 0.9 Strongly mineralized interval. Coincident with interval of sericitic alteration. Quartz-sericite-pyrite (QSPalteration assemblage? Mineralization also seen in microfractures.

205.04 207.74 0.3 interval of weaker mineralization. Dominant style is vein-hosted pyrite.207.74 209.10 0.6 Zone of relatively strong mineralization, generally disseminated (QSP?). Strongest chalcopyrite is

observed in quartz-plagioclase veinlets/dykelets.209.10 212.90 0.1 Weak to barren mineralization. No chalcopyrite observed, minor pyrite.212.90 224.95 Generally low-grade mineralization. Pyrite seen most commonly in microfractures (late?). Minor

chalcopyrite found in quartz-feldspar veins. Increase in sulphide abundance towards the bottom of the interval.

224.95 238.83 0.7 Mineralization dominated by disseminated pyrite, coinciding with sericitic zones (QSP). 238.83 274.05 Low grade vein-style mineralization. Improved pyrite-chalcopyrite tenor.274.05 279.65 0.44 Interval of strong copper mineralization. Dominant mineralization is vein-style, hosted by early quartz

veining, or remobilized in late gypsum veins. Local QSP-style disseminations.279.65 304.50 0.1 Weakly mineralized zone with good pyrite:copper tenor. Mineralization dominantly vein-hosted. Epidote

veins mineralized locally.304.50 307.05 0.3 Strongly pyrite mineralized interval. Chalcopyrite in trace amounts. The majority of mineralization is rel

to epidote vein networks.307.05 335.40 0.2 Mineralization dominated by epidote vein-hosted pyrite. Lesser chalcopyrite, also vein-hosted.335.40 346.91 0.05 Nearly barren rock. Trace pyrite locally.

KL06_31 10 May 2007 Page 6 of 14

346.91 377.25 0.2 Moderately mineralized interval. Dominant mineralization style is vein-hosted, with local patches of quasericite-pyrite alteration featuring disseminated pyrite. Mineralized vein styles include quartz, magnetiteand epidote.

391.56 398.70 0.25 Moderately mineralized interval. Dominantly vein-hosted pyrite. Local, restricted QSP.398.70 400.25 0.8 Abundant disseminated pyrite. Local quartz veins with chalcopyrite. Quartz-sericite-pyrite assemblage

(QSP).400.25 407.60 0.25 Moderately mineralized interval. Dominantly vein-hosted pyrite. Local, restricted QSP.407.60 411.38 0.8 Abundant disseminated pyrite. Local quartz veins with chalcopyrite. Quartz-sericite-pyrite assemblage

(QSP).411.38 422.93 0.25 Moderately mineralized interval. Dominantly vein-hosted pyrite. Local, restricted QSP.422.93 426.11 0.8 Abundant disseminated pyrite. Local quartz veins with chalcopyrite. Quartz-sericite-pyrite assemblage

(QSP).

StructureFrom To Int.m Struct 1 DescriptionAngle Int.Struct 2 Angle Int.Struct 3 Angle

13.72 38.80 ZRO INT Core is rubbled almost to a gravelly consistency.38.80 44.93 ZRO STG Core is strongly rubbled, with local portions of better-preserved material, although even these

portions are calcite veined.44.93 70.26 ZRO INT Core is rubbled almost to a gravelly consistency.70.26 73.90 ZRO STG Core is more competent than surrounding rubble, although still fractured strongly.73.90 90.28 ZRO INT Core is rubbled almost to a gravelly consistency.90.28 164.01 ZRO MOD Structure in this interval is weak to moderate. Open fractures are much less commonplace tha

in overlying intervals. Fracture veining commonplace.164.01 167.34 ZRO STG Core is strongly rubbled, in comparison to overlying rocks. Fracture veining still commonplace.167.34 171.05 ZRO MOD Structure in this interval is weak to moderate. Rare open fractures. Fracture veining

commonplace.171.05 171.90 ZFG MOD Local possible fault gouge observed. Clayey, finely ground material.171.90 229.63 ZRO MOD Structure in this interval is weak to moderate. Rare open fractures. Fracture veining

commonplace.229.63 230.50 ZFG MOD Local possible fault gouge observed. Clayey, finely ground material.230.50 238.83 SFS STG Locally strong fabric- ductile shearing?238.83 322.25 ZRO WK Structure for this interval is fairly weak, consisting mainly of fracture veining with rare open

fractures.322.25 332.25 ZRO MOD Relatively high density of open fractures.332.25 355.05 ZRO WK Structure for this interval is fairly weak, consisting mainly of fracture veining with rare open

fractures.355.05 357.10 ZRO STG Abundant open fractures. Core is approaching a rubbly state.357.10 378.80 ZRO MOD Core is relatively intact, although commonly fracture-veined.378.80 384.00 ZRO STG Rubbly core.384.00 408.35 ZRO MOD Core is relatively intact, although commonly fracture-veined.408.35 409.03 ZFG STG Possible fault gouge- clayey, ground rock.409.03 417.27 ZRO MOD Core is relatively intact, although commonly fracture-veined.417.27 417.49 ZRO STG "Cave"- rubble.417.49 426.11 ZRO MOD Core is relatively intact, although commonly fracture-veined.

KL06_31 10 May 2007 Page 7 of 14

Depth Beta Dip/Plunge

Feature Width DescriptionPoint Structure

AlphaDip/Plunge Dir.

m Gamma Reliability

173.22 355.0ZVS Sulphide veinlet- pyrite with trace chalcopyrite. Hosted by early quartz vein.2 43.0173.89 200.0ZVO Late gypsum fracture veinlet.0.4 30.0177.82 320.0ZVO Thick, late gypsum vein.2.5 18.0178.87 345.0ZVS Early, undulose sulphide veinlet, pyrite-dominated. Associated with gypsum (later, deposited

along the same fracture plane?).0.8 22.0

186.12 80.0ZVC Relatively late calcite veinlet, with lesser associated chlorite- syn-metamorphic (?).1 23.0187.96 100.0ZVC Thin calcite veinlet with associated chlorite.0.2 30.0188.89 75.0ZVO Gypsum-chlorite-pyrite veinlet. Sericitic selvage. Similar vein 5 cm uphole. Multiple vein phas

along the same pathway?0.8 53.0

191.04 125.0ZVQ Quartz-magnetite veinlet. Nearby chalcopyrite, possibly associated. Truncated/offset by a calcveinlet.

0.2 50.0

200.21 270.0ZVS Quartz-pyrite vein. Crosscut by gypsum1.5 52.0200.56 130.0ZVS Quartz-pyrite-magnetite vein. Pyritic vein core. 1.2 65.0202.99 35.0ZVS Quartz-pyrite vein. 1.5 70.0204.30 350.0ZVS Quartz-pyrite vein.2.3 58.0207.43 140.0ZVO quartz-carbonate-pyrite vein with sericitic selvage. Cut by gypsum.1 52.0208.46 293.0ZFG Clayey fault gouge.0.8 25.0242.83 50.0ZVQ Quartz-pyrite vein.1.2 25.0245.56 20.0ZVQ Quartz-pyrite vein.2.3 35.0246.45 5.0ZVO Late gypsum fracture veinlet.0.3 45.0247.36 340.0ZVO Quartz-sericite-pyrite (QSP) zone.3.5 30.0250.58 355.0ZVQ Quartz veinlet with sericitic/bleached selvage.0.4 50.0251.59 265.0ZVO Open fracture with gypsum coating.0.3 40.0253.11 30.0ZVQ Quartz-plagioclase-pyrite veinlet/dykelet.1.3 43.0253.64 55.0SFO Subtle fabric.10 44.0255.61 55.0SFO Subtle fabric- imparted by alignment of narrow, parallel, quartz veinlets.10 40.0257.38 355.0ZVO Quartz-gypsum-pyrite veinlet.0.8 20.0259.45 140.0ZVQ Quartz-pyrite-gypsum. Multiple vein phases along a common conduit?3.4 45.0262.22 150.0ZVQ Narrow late quartz veinlet.0.15 52.0263.67 270.0ZVQ Quartz-chlorite-calcite veinlet. Multiphase?0.8 36.0265.26 140.0ZVQ Quartz-plagioclase-pyrite veinlet/dykelet.0.3 30.0265.63 200.0ZVS Pyrite-gypsum veinlet. Remobilized pyrite.0.25 25.0269.50 40.0ZVO Gypsum veinlet containing remobilized chalcopyrite.0.8 40.0272.48 270.0ZVO Narrow, early magnetite veinlet0.2 54.0274.24 232.0ZVS Pyrite-gypsum veinlet. Remobilized pyrite. 1.2 42.0276.17 50.0ZVC Narrow calcite veinlet. Sericitic selvage.0.3 45.0276.90 80.0ZVS Sulphidic zone (QSP?).4.5 46.0279.15 290.0ZVS Zone with abundant chalcopyrite. Sericitic halo.3 15.0284.67 272.0ZVC Calcite vein, accessory chlorite. Associated gypsum (later vein phase).1.2 28.0285.60 305.0ZVC Calcite vein with accessory chlorite and minor sulphides.1.1 25.0287.51 262.0ZVC Calcite vein with accessory chlorite.2 54.0

KL06_31 10 May 2007 Page 8 of 14

SamplesFrom To Sample typeSample ID Cu_ppm Au_ppb Mo_ppm Pb_ppm Zn_ppm As_ppm Ag_ppm Hg_ppm Sb_ppmK_ppm Bi_ppm S_%

13.71 16.00 410227 CORE_HALF 452.69 56.3 13.33 30.14 465.9 8.8 0.699 0.038 0.31800 0.05 1.05

16.00 18.00 410228 CORE_HALF 899.03 113 35.61 49.82 1704.5 12.1 1.493 0.434 0.341900 0.09 1.8

18.00 20.00 410229 CORE_HALF 329.18 89.3 5.38 168.57 2057.7 16.4 0.781 0.598 0.381800 0.07 2.33

20.00 22.00 410231 CORE_HALF 884.3 135.3 3.51 39.14 1713.7 16.6 1.432 0.454 0.471400 0.05 2.67

22.00 24.00 410232 CORE_HALF 1612.21 173.7 25.44 31.06 378.9 21.9 2.612 0.04 0.52000 0.17 1.64

24.00 26.00 410233 CORE_HALF 483.54 46.8 9.08 79.82 318.7 31 0.841 0.016 1.041500 0.19 2.87

26.00 28.00 410234 CORE_HALF 388.53 45.2 13.99 11.79 244.7 15.8 0.468 0.006 0.241800 0.13 3.1

28.00 34.00 410235 CORE_HALF 174.88 34 3.33 11.59 259.6 7.4 0.284 -0.005 0.221700 0.1 2.9

34.00 36.00 410236 CORE_HALF 185.14 57.5 3.31 28.99 474.4 10 0.376 0.062 0.272100 0.14 2.48

36.00 38.00 410237 CORE_HALF 437.62 20.3 6.26 7.13 168.9 14.7 0.467 -0.005 0.161500 0.11 3.17

38.00 40.00 410238 CORE_HALF 88.46 23.9 2.06 12.12 121.3 5.1 0.228 -0.005 0.14200 0.06 0.5

40.00 42.00 410239 CORE_HALF 150.83 19.7 1.38 10.51 217 4.6 0.223 -0.005 0.1700 0.08 1.89

42.00 44.00 410240 CORE_HALF 137.78 19.6 1.01 4.85 218.1 8.6 0.17 -0.005 0.3300 0.05 0.83

44.00 46.00 410241 CORE_HALF 154.63 28.3 2.86 3.83 168 11.9 0.232 -0.005 0.26800 0.06 1.57

46.00 48.00 410242 CORE_HALF 155.94 18.2 1.96 3.03 176.4 10.5 0.222 -0.005 0.231000 0.04 1.54

48.00 50.00 410243 CORE_HALF 159.73 23.1 1.44 4.24 157.4 11.7 0.27 -0.005 0.21800 0.08 2.46

50.00 52.00 410244 CORE_HALF 266.32 29.1 6.91 4.18 169.1 10.6 0.461 -0.005 0.21600 0.1 3.68

52.00 54.00 410245 CORE_HALF 797.54 36.4 8.77 4.06 120.2 6.4 0.827 -0.005 0.181500 0.08 1.97

54.00 56.00 410246 CORE_HALF 256.37 22.9 3.24 2.94 97.1 4.2 0.313 -0.005 0.141400 0.11 3.73

56.00 60.00 410247 CORE_HALF 295.34 45.6 4.4 3.4 93.8 4.1 0.372 -0.005 0.131500 0.1 4.21

60.00 68.00 410248 CORE_HALF 356.7 32 3.84 4.64 103.4 4.9 0.355 -0.005 0.141600 0.12 2.98

68.00 70.00 410249 CORE_HALF 1533.77 95.8 7.83 5.07 90 12.9 1.221 -0.005 0.152000 0.29 3.69

70.00 72.00 410251 CORE_HALF 57.79 22.9 0.38 3.93 70.7 1.6 0.197 -0.005 0.1900 0.04 0.35

72.00 74.00 410252 CORE_HALF 46.17 12.5 0.2 3.47 69.4 1 0.117 -0.005 0.08900 0.02 0.09

74.00 76.00 410253 CORE_HALF 216.61 15 2.8 2.52 86.4 2.8 0.258 -0.005 0.161000 0.09 2.03

76.00 78.00 410254 CORE_HALF 150.74 8.3 4 2.27 108.6 2.9 0.108 -0.005 0.131200 0.12 2.98

78.00 80.00 410255 CORE_HALF 462.57 17.8 5.69 2.65 105.2 6.2 0.3 -0.005 0.151300 0.19 3.92

80.00 82.00 410256 CORE_HALF 329.64 81 5.6 2.44 100 4.8 0.315 -0.005 0.21300 0.14 2.9

82.00 84.00 410257 CORE_HALF 141.4 21.1 0.17 1.16 113.3 3 0.183 -0.005 0.33100 0.02 0.04

84.00 90.00 410258 CORE_HALF 411.8 36.4 2.59 1.53 79.9 2.5 0.339 -0.005 0.291000 0.1 1.77

90.00 92.00 410259 CORE_HALF 247.52 20.5 2.25 2.16 51.7 3 0.186 -0.005 0.141100 0.12 4.74

92.00 94.00 410260 CORE_HALF 495.8 37.7 5.29 2.1 48.2 3.3 0.373 -0.005 0.191000 0.13 5.64

94.00 96.00 410261 CORE_HALF 124.97 12.4 1.92 1.31 29.7 1.4 0.093 -0.005 0.131300 0.1 5.83

96.00 98.00 410262 CORE_HALF 542.86 51.9 4.13 1.58 50 2.2 0.385 -0.005 0.25800 0.1 3.21

98.00 100.00 410263 CORE_HALF 142.93 21.1 2.25 1.63 64.9 1.7 0.181 -0.005 0.25800 0.1 2.79

KL06_31 10 May 2007 Page 9 of 14

100.00 102.00 410264 CORE_HALF 734.49 66.2 4.61 2.15 38 1.5 1.056 0.008 0.371600 0.14 4.6

102.00 104.00 410265 CORE_HALF 417.75 31.1 3.55 1.24 43.7 1.4 0.344 -0.005 0.151200 0.05 2.88

104.00 106.00 410266 CORE_HALF 178.61 26.4 0.86 1.59 56.9 0.6 0.189 -0.005 0.13600 -0.02 1.27

106.00 108.00 410267 CORE_HALF 419.16 26.7 1.49 2.22 67.5 0.7 0.305 -0.005 0.09700 0.05 1.7

108.00 110.00 410268 CORE_HALF 711.21 53.8 1.35 1.34 62.2 0.8 0.414 -0.005 0.13900 0.03 1.49

110.00 112.00 410269 CORE_HALF 2797.53 199.6 2.17 1.26 60.6 0.9 1.521 0.006 0.161200 0.04 2.44

112.00 114.00 410271 CORE_HALF 323.97 22.8 0.91 1.4 58.4 0.6 0.2 -0.005 0.091100 0.03 0.89

114.00 116.00 410272 CORE_HALF 1976.58 181.5 1.35 2.59 67.1 1.7 1.378 0.007 0.111000 0.14 1.35

116.00 118.00 410273 CORE_HALF 1871.74 234.6 3.4 2.53 52.1 1.5 1.806 0.007 0.111400 0.16 3.5

118.00 120.00 410274 CORE_HALF 1786.71 156.6 17.65 1.64 58.5 1.3 1.166 -0.005 0.151000 0.12 3.43

120.00 122.00 410275 CORE_HALF 1702.06 172.2 8.21 1.72 76.5 1.2 1.188 -0.005 0.151100 0.13 2.83

122.00 124.00 410276 CORE_HALF 637.91 79.2 4.46 1.7 55.3 1.1 0.482 -0.005 0.1900 0.13 3.52

124.00 126.00 410277 CORE_HALF 746.33 69.6 3.48 1.88 62.9 1.5 0.466 -0.005 0.151400 0.07 2.81

126.00 128.00 410278 CORE_HALF 948.54 59.4 1.53 1.38 77.5 1.4 0.606 0.007 0.191000 0.06 3.28

128.00 130.00 410279 CORE_HALF 876.84 100.9 1.61 1.82 72.6 0.8 0.53 0.012 0.21200 0.04 3.96

130.00 132.00 410280 CORE_HALF 886.71 124.1 3.41 2.71 62.9 1.2 0.641 -0.005 0.161300 0.05 3.25

132.00 134.00 410281 CORE_HALF 760.55 69.1 3.21 1.95 69.5 1.4 0.417 0.006 0.111100 0.13 2.89

134.00 136.00 410282 CORE_HALF 920.57 70.8 2.4 1.52 76.3 0.8 0.498 -0.005 0.09900 0.06 2.74

136.00 138.00 410283 CORE_HALF 985.43 100.4 1.43 1.85 146.1 0.8 0.64 0.006 0.11900 0.08 2.01

138.00 140.00 410284 CORE_HALF 3103.29 971.6 1.57 1.78 75.4 0.9 2.263 -0.005 0.15800 0.17 1.95

140.00 142.00 410285 CORE_HALF 5033.73 746.4 6.5 2.64 61.8 0.9 2.199 -0.005 0.211100 0.25 2.98

142.00 144.00 410286 CORE_HALF 3675.29 578.7 2.8 1.86 76.9 1 2.815 -0.005 0.21900 0.15 1.65

144.00 146.00 410287 CORE_HALF 2455.44 503.8 1.72 2.14 94.1 1.1 2.188 -0.005 0.12800 0.18 2.02

146.00 148.00 410288 CORE_HALF 1788.24 330.4 2.65 2.01 97.1 1 1.647 -0.005 0.09900 0.27 2.05

148.00 150.00 410289 CORE_HALF 932.38 203.2 3.13 1.88 46.4 1.1 1.491 0.014 0.11300 0.27 2.66

150.00 152.00 410291 CORE_HALF 925.76 367.4 4.5 2.12 26.6 1 1.875 0.015 0.11500 0.27 2.66

152.00 154.00 410292 CORE_HALF 1245.88 132.3 19.62 1.64 30.4 3.1 0.818 -0.005 0.071100 0.13 2.46

154.00 156.00 410293 CORE_HALF 1679.01 278 2.54 1.4 41.1 1.4 1.348 -0.005 0.071100 0.11 1.49

156.00 158.00 410294 CORE_HALF 1355.13 268.8 1.48 1.77 40.7 1.1 0.88 -0.005 0.051000 0.13 1.64

158.00 160.00 410295 CORE_HALF 1346.59 151.1 4.29 4.77 49 0.7 1.911 0.006 0.061200 0.07 1.13

160.00 162.00 410296 CORE_HALF 746.77 788 34.81 1.72 36.1 0.5 0.938 -0.005 0.051100 0.24 1.65

162.00 164.00 410297 CORE_HALF 811.26 290.5 6.22 1.49 45 0.4 0.642 -0.005 0.061400 0.14 1.34

164.00 166.00 410298 CORE_HALF 246.56 49 0.85 3.49 60.1 0.5 0.37 -0.005 0.11300 0.07 0.37

166.00 168.00 410299 CORE_HALF 923.63 256.6 2.3 2.01 52.8 0.5 2.083 0.005 0.071400 0.09 1.39

168.00 170.00 410300 CORE_HALF 883.24 166.2 3.45 1.8 42.8 0.9 0.759 -0.005 0.051400 0.07 1.11

170.00 172.00 410301 CORE_HALF 433.27 147.8 0.93 3.22 62.8 0.5 1.24 0.013 0.051300 0.08 0.82

172.00 174.00 410302 CORE_HALF 1268.17 633.1 2.81 2.04 46.3 1.6 2.105 0.007 0.1900 0.22 1.32

KL06_31 10 May 2007 Page 10 of 14

174.00 176.00 410303 CORE_HALF 1021.83 202.6 0.99 2.14 46 3.8 0.806 -0.005 0.231200 0.17 1.15

176.00 178.00 410304 CORE_HALF 613.78 109.9 1.51 1.72 25.1 2.8 0.552 -0.005 0.15600 0.24 6.22

178.00 180.00 410305 CORE_HALF 1381.1 273.7 0.82 1.37 39.4 1.8 1.026 -0.005 0.151200 0.1 1.26

180.00 182.00 410306 CORE_HALF 1395.21 340.5 0.59 1.45 48.2 2.1 1.404 0.008 0.161200 0.19 1.34

182.00 184.00 410307 CORE_HALF 1110.04 373.8 0.66 1.31 48.7 1 0.872 0.006 0.12800 0.09 0.76

184.00 186.00 410308 CORE_HALF 1020.88 413.6 0.68 1.25 52.6 1.4 0.702 -0.005 0.12800 0.13 0.94

186.00 188.00 410309 CORE_HALF 668.8 330.5 0.82 0.89 52.2 1.1 0.443 -0.005 0.13600 0.08 0.59

188.00 190.00 410311 CORE_HALF 491.57 102.4 0.72 0.66 51.4 1.2 0.32 -0.005 0.1400 0.06 0.52

190.00 192.00 410312 CORE_HALF 776 184.1 1.3 1.03 53.9 0.7 0.582 -0.005 0.11600 0.06 0.43

192.00 194.00 410313 CORE_HALF 500.84 104.6 1.23 0.95 48.9 1.4 0.465 -0.005 0.09600 0.08 0.54

194.00 196.00 410314 CORE_HALF 241.1 73.4 0.73 1.06 45.3 0.8 0.214 -0.005 0.091200 0.14 0.77

196.00 198.00 410315 CORE_HALF 193.57 176.3 0.85 2.28 30.8 0.6 1.414 -0.005 0.091100 0.21 4.46

198.00 200.00 410316 CORE_HALF 314.3 145.2 0.54 1.3 41 1.1 0.304 -0.005 0.131000 0.21 0.93

200.00 202.00 410317 CORE_HALF 197.92 413.2 2.21 0.88 31.8 0.6 2.187 -0.005 0.071200 0.2 1.75

202.00 204.00 410318 CORE_HALF 203.58 512.1 0.46 1.06 20 0.3 2.94 0.005 0.081100 0.32 3.58

204.00 206.00 410319 CORE_HALF 267.04 697.7 1.97 1.14 17.1 0.8 2.963 0.006 0.111000 0.32 3.17

206.00 208.00 410320 CORE_HALF 297.12 153.6 1.07 0.99 27.3 0.7 0.638 -0.005 0.091000 0.22 1.17

208.00 210.00 410321 CORE_HALF 578.26 480.3 2.33 1.4 28.4 0.9 2.109 -0.005 0.131100 0.39 2.77

210.00 212.00 410322 CORE_HALF 327.39 57.3 0.73 0.83 51.2 0.7 0.166 -0.005 0.1700 0.07 0.94

212.00 214.00 410323 CORE_HALF 169.77 67 0.56 0.95 41.3 2.2 0.14 -0.005 0.08700 0.09 1.39

214.00 216.00 410324 CORE_HALF 148.77 52.3 0.5 1.14 39.8 3 0.199 -0.005 0.1900 0.09 0.93

216.00 218.00 410325 CORE_HALF 171.66 44.1 0.58 1.23 47.6 2.3 0.141 -0.005 0.11600 0.08 0.57

218.00 220.00 410326 CORE_HALF 235.36 61.3 1.42 1.06 54.2 0.7 0.24 -0.005 0.09500 0.06 0.83

220.00 222.00 410327 CORE_HALF 263.35 97 0.92 1.16 47.5 3.7 0.418 -0.005 0.09700 0.21 1.22

222.00 224.00 410328 CORE_HALF 814.35 235.9 1.08 1.58 39 6.4 0.612 -0.005 0.13800 0.22 1.28

224.00 226.00 410329 CORE_HALF 295.65 225.6 6.03 2.17 34.4 3.2 0.747 -0.005 0.151700 0.31 2.53

226.00 228.00 410331 CORE_HALF 80.35 2863.7 1.74 10.53 15.1 3.5 5.507 -0.005 0.471700 2.1 5.79

228.00 230.00 410332 CORE_HALF 198.67 787 2.54 10.23 19.3 2.1 3.455 -0.005 0.291500 0.88 3.37

230.00 232.00 410333 CORE_HALF 1717.05 627.9 17.57 8.33 67.5 0.9 8.135 -0.005 0.341700 0.65 4.02

232.00 234.00 410334 CORE_HALF 2103.31 657.4 0.69 4.38 147.2 0.6 3.628 -0.005 0.381000 0.23 2.4

234.00 236.00 410335 CORE_HALF 267.77 132.5 0.6 6.45 48.6 1.6 1.092 -0.005 0.241700 0.09 1.88

236.00 238.00 410336 CORE_HALF 365.76 345.7 0.8 9.4 43.5 2.4 3.279 -0.005 0.951300 0.17 5.19

238.00 240.00 410337 CORE_HALF 785.69 295.7 1.4 2.97 65.3 1.6 1.526 -0.005 0.61100 0.12 2.44

240.00 242.00 410338 CORE_HALF 1425.67 391.5 1.28 1.6 69.8 1.9 1.025 -0.005 0.28800 0.17 1.22

242.00 244.00 410339 CORE_HALF 1318.03 383.5 1.26 1.6 81.8 0.6 1.025 -0.005 0.341100 0.09 1.53

244.00 246.00 410340 CORE_HALF 953.8 375.5 1.85 1.66 75.8 1.3 1.049 -0.005 0.281100 0.11 1.24

246.00 248.00 410341 CORE_HALF 361.12 366.9 7.33 2.71 65.2 1.8 0.865 -0.005 0.361200 0.12 2.97

KL06_31 10 May 2007 Page 11 of 14

248.00 250.00 410342 CORE_HALF 110.89 26.1 0.56 2.14 44.9 1.2 0.118 -0.005 0.231800 0.05 0.65

250.00 252.00 410343 CORE_HALF 223.7 60 0.72 2.65 48.3 3.1 0.233 -0.005 0.252000 0.09 0.82

252.00 254.00 410344 CORE_HALF 553.51 198 0.65 2.76 56.6 7.3 0.643 -0.005 0.272100 0.08 1.11

254.00 256.00 410345 CORE_HALF 1022.71 356.4 0.61 1.97 90.8 0.7 1.432 -0.005 0.161400 0.07 1.29

256.00 258.00 410346 CORE_HALF 905.05 212.5 1.64 1.35 66.3 1.4 0.481 -0.005 0.12900 0.17 2.09

258.00 260.00 410347 CORE_HALF 714.05 152.5 0.65 1.25 50.6 0.5 0.368 -0.005 0.1900 0.08 1.35

260.00 262.00 410348 CORE_HALF 1155.19 204.2 0.44 1.09 47.5 0.3 0.606 -0.005 0.11800 0.05 0.86

262.00 264.00 410349 CORE_HALF 1118.08 168.8 0.57 1.84 45.6 0.2 1.779 0.006 0.11200 0.09 1.05

264.00 266.00 410351 CORE_HALF 2017.6 335.1 0.82 1.58 54.5 1.2 2.569 0.005 0.121200 0.35 1.87

266.00 268.00 410352 CORE_HALF 668.93 128.5 1.87 1.85 64.3 0.4 0.339 -0.005 0.11800 0.03 1

268.00 270.00 410353 CORE_HALF 422.81 106.9 0.75 1.82 71.5 0.7 0.883 0.011 0.11000 0.17 2.02

270.00 272.00 410354 CORE_HALF 481.4 76.8 0.9 1.79 60.2 0.8 0.353 0.006 0.111000 0.04 1.21

272.00 274.00 410355 CORE_HALF 367.31 104.5 0.66 2.06 48.6 0.9 0.298 -0.005 0.121100 0.07 1.2

274.00 276.00 410356 CORE_HALF 3248.29 341.5 0.74 4.4 51.2 0.6 3.528 0.016 0.231300 0.36 2.76

276.00 278.00 410357 CORE_HALF 5853.72 435.2 1.02 2.19 49.2 -0.1 5.805 0.005 0.181000 0.41 2.4

278.00 280.00 410358 CORE_HALF 15790 516.2 2.73 2.72 37 0.3 11.189 0.012 0.36600 1.11 5.13

280.00 282.00 410359 CORE_HALF 1171.08 159.1 0.87 1.47 81.5 1.1 0.819 0.007 0.151000 0.13 1.13

282.00 284.00 410360 CORE_HALF 1859.82 259.6 1 1.98 77.1 1 1.008 -0.005 0.21000 0.07 1.5

284.00 286.00 410361 CORE_HALF 828.97 204.1 0.63 1.89 75.4 1 0.709 -0.005 0.16900 0.1 1.19

286.00 288.00 410362 CORE_HALF 1010.21 184.8 0.56 2.19 70.5 0.9 0.59 -0.005 0.131600 0.07 0.62

288.00 290.00 410363 CORE_HALF 750.37 115 15.18 1.34 55.3 1 0.427 -0.005 0.11300 0.04 0.96

290.00 292.00 410364 CORE_HALF 456.26 47.1 89.12 1.46 45.6 0.8 0.286 -0.005 0.11500 0.04 0.72

292.00 294.00 410365 CORE_HALF 620.68 52.6 1.65 1.15 59.9 1.7 0.367 -0.005 0.071200 0.05 1.26

294.00 296.00 410366 CORE_HALF 826.96 74.6 1.85 1.5 66.1 1.2 0.48 -0.005 0.112000 0.11 1.1

296.00 298.00 410367 CORE_HALF 364.4 23.9 0.92 1.66 65.8 1.1 0.307 -0.005 0.151500 0.06 1.83

298.00 300.00 410368 CORE_HALF 175.29 15.1 5.02 0.93 80.1 1.2 0.204 -0.005 0.081400 0.03 1.02

300.00 302.00 410369 CORE_HALF 1020.65 86.4 0.85 1.04 69.2 1.2 0.415 -0.005 0.131800 0.07 1.9

302.00 304.00 410371 CORE_HALF 1107.81 100.1 0.91 1.19 77.7 1 0.508 -0.005 0.111100 0.03 0.91

304.00 306.00 410372 CORE_HALF 1049.7 84.1 9.55 2.2 68.2 2.6 0.627 0.011 0.21300 0.38 4.77

306.00 308.00 410373 CORE_HALF 429.7 38.6 1.02 1.32 74 1.9 0.193 -0.005 0.192700 0.08 1.1

308.00 310.00 410374 CORE_HALF 318.63 41.6 1.18 1.06 78.6 1 0.175 -0.005 0.172600 0.03 0.74

310.00 312.00 410375 CORE_HALF 372.28 49.4 0.95 1.46 77.9 1.2 0.288 0.007 0.262700 0.06 1.13

312.00 314.00 410376 CORE_HALF 686.63 76.7 0.64 0.94 82.8 1.2 0.361 -0.005 0.122500 0.02 0.62

314.00 316.00 410377 CORE_HALF 914.82 122.1 0.59 2.6 83.3 0.8 0.508 -0.005 0.114200 0.02 0.36

316.00 318.00 410378 CORE_HALF 624.04 123.9 0.99 0.98 74.4 2.5 0.389 0.005 0.112700 0.13 1.37

318.00 320.00 410379 CORE_HALF 306.51 47.4 2.52 1.04 51 0.8 0.168 -0.005 0.12200 0.03 1.72

320.00 322.00 410380 CORE_HALF 652.56 113.4 1.05 1.43 43.9 2.8 0.362 0.014 0.111900 0.1 1.93

KL06_31 10 May 2007 Page 12 of 14

322.00 324.00 410381 CORE_HALF 252.4 49.2 0.61 1.02 42.8 1 0.147 0.011 0.092600 0.06 1.34

324.00 326.00 410382 CORE_HALF 365.21 82.9 2.18 1.83 80.2 6.9 0.238 0.006 0.126500 0.11 1.28

326.00 328.00 410383 CORE_HALF 1927.18 416.6 0.51 1.34 53.4 1.8 0.877 0.009 0.141600 0.1 1.06

328.00 330.00 410384 CORE_HALF 2113.91 391.4 0.41 1.14 60.9 1.4 0.944 0.008 0.11700 0.1 0.63

330.00 332.00 410385 CORE_HALF 4281.99 691.2 0.54 1.25 58.6 0.8 2.24 0.02 0.171600 0.17 1.57

332.00 334.00 410386 CORE_HALF 1401.79 353.1 0.43 1.05 64.6 1.4 0.952 0.023 0.121700 0.12 1.04

334.00 336.00 410387 CORE_HALF 1069.01 262.2 0.27 1.28 65.4 1.1 0.725 -0.005 0.082800 0.07 0.42

336.00 338.00 410388 CORE_HALF 41.87 22.7 0.07 1.82 56.6 0.9 0.046 -0.005 0.085700 0.03 0.17

338.00 340.00 410389 CORE_HALF 34.25 7.3 0.08 2.45 54.7 1 0.075 0.005 0.089300 0.02 0.14

340.00 342.00 410391 CORE_HALF 31.43 5.6 0.07 1.96 55.6 0.5 0.036 -0.005 0.057400 0.02 0.09

342.00 344.00 410392 CORE_HALF 29.23 3.5 0.08 1.88 51.5 0.3 0.031 -0.005 0.047100 -0.02 0.09

344.00 346.00 410393 CORE_HALF 28.62 6 0.53 173.69 81.4 15 1.077 -0.005 1.247300 0.04 0.13

346.00 348.00 410394 CORE_HALF 1701.84 369.9 0.92 1.63 54.7 1 0.938 0.011 0.073800 0.18 1.46

348.00 350.00 410395 CORE_HALF 3475.35 964.5 0.48 27.82 54.1 2.1 1.657 0.011 0.2800 0.2 0.67

350.00 352.00 410396 CORE_HALF 2759 609.3 0.35 0.88 47.9 -0.1 1.09 0.014 0.07700 0.11 0.44

352.00 354.00 410397 CORE_HALF 4729.35 1307.6 0.75 15.51 52.7 1.7 2.004 0.02 0.14800 0.25 1.34

354.00 356.00 410398 CORE_HALF 3222.69 858.2 0.54 0.87 54.9 0.5 1.513 0.016 0.111700 0.16 0.6

356.00 358.00 410399 CORE_HALF 2709.8 889 0.34 0.96 65 0.4 1.324 0.01 0.08900 0.15 0.43

358.00 360.00 410400 CORE_HALF 1392.5 371.9 3.24 0.93 39.9 0.8 0.999 0.01 0.091400 0.14 0.89

360.00 362.00 410401 CORE_HALF 2384.28 642.6 0.27 1.07 42.2 0.3 0.982 -0.005 0.15900 0.15 0.39

362.00 364.00 410402 CORE_HALF 1645.16 340.2 1.15 1.02 41.8 0.2 0.698 -0.005 0.1800 0.08 0.64

364.00 366.00 410403 CORE_HALF 1635.62 430.2 14 0.95 41.8 0.1 0.751 0.007 0.1900 0.09 0.75

366.00 368.00 410404 CORE_HALF 1759.51 525.1 1.4 0.79 37.3 0.8 1.023 0.013 0.11000 0.13 1.69

368.00 370.00 410405 CORE_HALF 1471.77 338.8 1.4 0.87 38.6 1.3 0.808 0.009 0.081000 0.1 1.42

370.00 372.00 410406 CORE_HALF 1914.36 522.7 14.21 0.77 42.3 0.8 1.079 0.009 0.11100 0.1 1.29

372.00 374.00 410407 CORE_HALF 2741.06 779.6 0.82 0.81 49.8 -0.1 1.509 0.013 0.111700 0.1 0.94

374.00 376.00 410408 CORE_HALF 583.76 182.1 0.36 1.96 68.2 0.3 0.346 0.005 0.12500 0.04 0.23

376.00 378.00 410409 CORE_HALF 46.6 817.9 0.15 3.22 67.5 2.6 0.137 0.006 0.133500 0.05 0.41

378.00 380.00 410411 CORE_HALF 29.29 52.1 0.11 2.39 80.6 1.2 0.065 0.005 0.093300 0.03 0.18

380.00 382.00 410412 CORE_HALF 30.87 6.7 0.11 2.45 73.7 0.7 0.049 -0.005 0.092900 0.02 0.19

382.00 384.00 410413 CORE_HALF 35.32 9.2 0.11 2.32 75.7 0.8 0.067 0.008 0.113700 0.02 0.11

384.00 386.00 410414 CORE_HALF 32.89 5 0.12 1.97 66.8 0.7 0.039 -0.005 0.084700 0.02 0.12

386.00 388.00 410415 CORE_HALF 56.87 12.8 0.15 2.65 64.2 0.5 0.049 -0.005 0.112800 0.03 0.2

388.00 390.00 410416 CORE_HALF 32.12 13.1 0.12 2.7 59.3 0.7 0.066 -0.005 0.092300 0.05 0.21

390.00 392.00 410417 CORE_HALF 254.13 104.5 0.99 1.63 53.8 1.2 0.214 -0.005 0.122600 0.06 0.57

392.00 394.00 410418 CORE_HALF 1238.23 482.6 0.65 0.84 29.2 1.6 0.553 0.008 0.071100 0.06 0.94

394.00 396.00 410419 CORE_HALF 675.29 233.6 0.44 0.89 35 1.3 0.638 0.007 0.081700 0.08 1.06

KL06_31 10 May 2007 Page 13 of 14

396.00 398.00 410421 CORE_HALF 645.66 233.1 0.66 0.68 32.2 0.9 0.375 0.005 0.061100 0.05 0.56

398.00 400.00 410422 CORE_HALF 3610.08 1522.1 0.97 0.78 33.6 1.1 1.611 0.024 0.08800 0.17 1.8

400.00 402.00 410423 CORE_HALF 795.22 310 0.5 0.82 30.3 1 0.428 0.006 0.051100 0.08 0.74

402.00 404.00 410424 CORE_HALF 1793.48 568 2.97 1.17 29.9 4.9 1.066 0.013 0.111300 0.23 2.61

404.00 406.00 410425 CORE_HALF 1137.32 422.3 0.74 1.24 24.5 3.9 0.597 -0.005 0.091500 0.11 1.75

406.00 408.00 410426 CORE_HALF 1460.11 1408.4 0.67 2.17 36.1 1.8 1.417 0.018 0.131500 0.68 3.49

408.00 410.00 410427 CORE_HALF 655.47 4059.8 2.71 2.74 17.3 0.9 2.514 0.026 0.111900 1.54 5.5

410.00 412.00 410428 CORE_HALF 163.05 119.9 0.59 1 19.8 1.5 0.128 0.006 0.072100 0.12 3.4

412.00 414.00 410429 CORE_HALF 2056.85 1147.4 0.27 1.1 25 0.3 1.078 -0.005 0.071400 0.06 1.1

414.00 416.00 410430 CORE_HALF 1897.66 792.5 4.54 1.74 31.6 0.4 2.441 0.016 0.061400 0.12 2.38

416.00 418.00 410431 CORE_HALF 877.51 1797.5 1.05 1.38 37.6 1 1.053 0.006 0.071500 0.41 3.13

418.00 420.00 410432 CORE_HALF 527.7 259.5 2.47 0.67 40.6 0.1 0.406 -0.005 0.05900 0.06 1.08

420.00 422.00 410433 CORE_HALF 313.99 160.4 1.99 0.57 32.4 0.1 0.206 -0.005 0.04600 0.05 1.78

422.00 424.00 410434 CORE_HALF 63.99 58.8 0.44 0.73 25.2 0.4 0.053 0.006 0.04900 0.08 2.66

424.00 426.11 410435 CORE_HALF 44.31 7.1 2.66 0.75 14.9 0.9 0.033 0.005 0.041300 0.07 3.3

KL06_31 10 May 2007 Page 14 of 14

GEOINFORMATICS REDTON LITHOLOGY CODES

INTRUSIVE lith code VOLCANIC lith code SEDIMENTS

lith

code METAMORPHIC

lith

code VOLCANICLASTIC

lith

code

ALTERED ROCKS

(original rock type unidentifiable)

lith

code OTHER

lith

code

Undifferentiated Intrusives IOO Undifferentiated Volcanic Rocks VOO Undifferentiated Sediments SOO Undifferentiated metamorphic rock XOO Undifferentiated Volcaniclastic Rocks YOO Altered Rock, Undivided AOO Unknown rock type OOO

porphyry, undiff. IOP Undifferentiated Volcanic Rocks - porphyritic VOP Conglomerate SCO Amphibolite, undivided XAO tuff - unknown composition YOT Altered intrusive rock AIO Unknown, missing interval, lost sample OMIUndifferentiated Felsic Intrusives IFO Undifferentiated Felsic Volcanic Rocks VFO Conglomerate - boulder SCB Gneiss, undivided XGO agglomerate - unknown composition YOA Altered volcanic rock AVO Unknown, not logged ONLPorphyritic felsic intrusive IFP Undifferentiated Felsic Volcanic Rocks - porphyritic VFP Conglomerate - pebble/cobble SCC granulite XGG ignimbrite - unknown composition YOI Altered sedimentary rock ASS Drill Casing CASE

Pegmatite, undivided IFPG Rhyolite VFR Conglomerate - granule SCG Ortho-gneiss XGI Undiff Felsic Volcaniclastics YFO Albite altered rock AAO

Granite IFG Rhyolite - quartz +/- feldspar phyric VFRP Conglomerate - polymictic SCP Migmatite XGM agglomerate felsic YFA Biotite alteration ABO SURFICIAL

Porphyritic granite IFGP Dacite VFD Conglomerate - monomictic SCM quartzofeldspathic gneiss XGQ ignimbrite - felsic YFI Carbonate-chlorite ACH Overburden OVER

adamellite IFGA Dacite - quartz +/- feldspar phyric VFDP Sedimentary Breccia (sharpstone Conglom.) SCX Para-gneiss XGS tuff - felsic YFT Carbonate altered rock ACO undivided regolith ROO

albite granite IFGB Rhyodacite VFRD clastic sediments (coarser than siltsize) SSO pelitic gneiss XGSP Rhyolite tuff YFR Fuchsite alteration AFO soil ROS

aplite IFA Undifferentiated Intermediate Volcanic Rocks VIO Sandstone/Arenite SSA psammitic gneiss XGSS Dacite tuff YFD Chloritic alteration AHO undivided residual regolith RRO

charnockite IFC Intermediate Volcanics - quartz +/- feldspar phyric VIOP Calcareous arenite/sandstone SSB eclogite XEO Undiff Intermediate Volcaniclastics YIO K-spar alteration AKO Transported colluvium RTC

Granodiorite IFD Intermediate Volcanics - vesicular/amygdaloidal VIOV Carbonaceous arenite/sandstone SSC Hornfels, undivided XHO agglomerate - intermediate YIA Silica-carbonate AQC undivided transported regolith RTO

Porphyritic granodiorite IFDP Andesite VIA Sulphidic arenite/sandstone SSZ dolomitic marble XLD ignimbrite - intermediate YII Silica-sericite AQE Unconsolidated alluvium RTA

Trondjhemite IFJ Andesite - quartz +/- feldspar phyric VIAP Arkose SSK marble XLO tuff - intermediate YIT Silica-fuchsite AQF gravel RTG

Tonalite IFT Andesite - amygdaloidal/vesicular VIAV Volcanic arenite/sandstone SSV Schist, undivided XSO andesite tuff YIAT Silica-chlorite AQH till RTT

Alkalic Intrusion, undivided IKO basaltic andesite VIB Quartzite SSQ Phyllite/slate, undivided XPO Undiff Mafic Volcaniclastics YMO Silica alteration AQO Gossan RGO

Syenite IKS trachyandesite VIT Wacke SWO Biotite schist XSB agglomerate - mafic YMA Sericite-Carbonate ASC FAULT ZONES

Porphyritic syenite IKSP Alkalic volcanic, undivided VKO Calcareous Greywacke SWB carbonate schist and calc-schist XSC ignimbrite - mafic YMI Sericitic alteration ASO Fault/Fault zone ZFO

nepheline syenite IKSN Alkalic volcanic - quartz +/- feldspar phyric VKOP Carbonaceous/graphitic Greywacke SWC feldspathic schist XSF tuff - mafic YMT Sericite-chlorite ASH fault gouge ZFG

quartz syenite IKSQ Latite (porphyritic) VKL Sulphidic Greywacke SWZ schist - graphitic XSG Sericite-clay ASL fault breccia ZFX

Albitite IKA alkali feldspar rhyolite VKR Siltstone SIO Chlorite schist XSH Clay alteration ALO Mylonite/tectonite ZMO

Carbonatite IKC Trachyte VKT Calcareous siltstone SIB sericite schist XSK Clay-chlorite ALH

alkali feldspar granite / syenogranite IKGF Undifferentiated Mafic Volcanic Rocks VMO Carbonaceous/graphitic siltstone SIC muscovite schist XSM Dominantly sulphide rock AZO VEINS

Shoshonite IKH Mafic lava; amygdaloidal/vesicular VMOV Quartzose/siliceous siltstone SIQ pelitic schist XSP vein, undifferentiated ZVOUndifferentiated Intermediate Intrusives IIO Basalt VMB Sulphidic siltstone SIZ psammitic schist XSS carbonate-dominant vein ZVCPorphyritic intermediate intrusive IIP Basalt - amygdaloidal/vesicular VMBV Argillite SAO Psammite, undivided XMO quartz-dominant vein ZVQ

Diorite IID Pillow basalt VMBP Calcareous argillite/shale/mudstone SAB meta-quartzite XQO quartz-carbonate dominant vein ZVQC

Porphyritic diorite intrusive IIDP olivine basalt VMBO Carbonaceous/graphitic argillite/shale/mudstone SAC Talc - Chlorite schist XST quartz-feldspar dominant vein ZVQF

Monzonite IIM Tholeitic basalt VMBT Quartzose/siliceous argillite SAQ meta-ultramafic undivided XUO sulphidic vein ZVS

Porphyritic monzonite intrusive IIMP komatiitic basalt VMK Sulphidic argillite/shale/mudstone SAZ serpentinite XUS

Quartz diorite IIQ Undifferentiated Ultramafic Volcanic Rocks VUO shale SIH

Porphyritic quartz diorite intrusive IIQP Komatiite VUK mudstone SIM

Quartz monzonite IIZ Peridotite VUP Chert STO

Porphyritic quartz monzonite intrusive IIZP Pyroxenite VUX Banded Iron Formation STF

Monzodiorite III sulphidic chert STZ

Porphyritic monzodiorite intrusive IIIP Carbonate sediments, undivided SLO

Undifferentiated Mafic Intrusives IMO Limestone SLL

Porphyritic mafic intrusive IMP Dolomite/Dolostone SLD

Gabbro IMG Biogenic rock, undifferentiated BOO

hornblende gabbro IMGH Biogenic carbonaceous deposit, undiff BCO

gabbronorite IMGN

olivine gabbro IMGO

Norite IMN

Troctolite IMT

Dolerite / Diabase IMD

Undifferentiated Ultramafic Intrusion IUO

Peridotite IUP

Picrite IUR

Pyroxenite IUX

clinopyroxenite IUXC

orthopyroxenite IUXO

Dunite IUD

Hornblendite IUH

Harzburgite IUZ

Undifferentiated lamprophyre ILO

GEOINFORMATICS REDTON VEINING CODES

Vein_style Vein_intensity Vein_mineral

Code

includes: style-geometry-

structure-size code code

use same code

abbreviation as for AGSO

minerals

BND Boudinaged Vein ( ) *absolute % UNK unknown

BRX Vein Breccia tr trace (<2%)

CKD Cockade Vein wk weak (2-10%) ACN acanthite

COL Colloform Vein mod moderate/medium (10-25%) ACT actinolite

CON Conjugate Veins stg strong (25-50%) ADU adularia

CRC Crackle Vein int intense (>50%) AEG aegirine

DRU Drusy unk unknown intensity AGT aegirine-augite

EEN En Echelon Veins AEN aenigmatite

EXT Extensional Vein When Recoding legacy data AIK aikinite

FELD Narrow felsic dyke/vein wk few AK akermanite

FMV Fine/micro-veins wk minor ALB alabandite

FOL Folded vein wk (+/-) AB albite

FRV Fracture Veins wk some ALN allanite

FTV Fault-related veins wk partly ALG allargentum

HLN Hairline Veins wk rare ALP allophane

INTD Narow intermediate dyke/vein wk scattered ALM almandine

IRR Irregular / undeformed / segmented wk patchy ALT altaite

LAC Laced veinlets wk irregular AKT aluminokataphorite

LAM Laminated Veins ALSI aluminosilicate (unspecified)

LAMD Narrow lamprophyre dyke/vein mod common ALU alunite

LIND Late intrusive dyke/stringer vein mod numerous AMB amblygonite

MAS Massive Veins mod many AMS amesite

NET Net-like veining mod regular AMPH amphibole

PEG Pegmatite Veins etc etc etc etc

PLN Planar Veins

PTY Ptygmatic folded veins

RIB Ribbon Veins

SHR Sheared Veins

SHT Sheeted Veins

SIG Sigmoidal Veins

SMS Seams

STK Stockwork Veins

STR Stringer Veins

STY Stylolitic

SYND Narrow syenitic dyke/vein

TEN Tension Gashes

UND Undifferentiated Veins / veinlets

WSP Wispy

GEOINFORMATICS REDTON STRUCTURE CODES

Drilling / hand specimen Data Mapping Data

CODE STRUCTURE_1 INTENSITY CODE DESCRIPTION

PRIMARY STRUCTURES FAA Fold axis - anticline

MAS massive undeformed tr trace FAAF Fold axis - antiform

SBO bedding / bedded wk weak FAAO Fold axis - overturned anticline

SBOO bedding overturned mod moderate/medium FAO Fold axis - undivided

SFB Primary surface - flow banding or cumulate banding stg strong FAP Fold - axial plane

YCH Younging - scour marks int intense FAS Fold axis - syncline

YDEN Younging - density structures unk unknown intensity FASF Fold axis - synform

YGB Younging - graded bedding FASO Fold axis - overturned syncline

YNG Younging - undivided When Recoding legacy data FFA Fold axis - undivided

YPIL Younging - pillows wk weak FTAC Fold - trace of anticline axial plane

YXB Younging - cross bedding wk poorly FTAF Fold - trace of antiform axial plane

wk (+/-) FTAO Fold - trace of overturned anticline axial plane

DUCTILE STRUCTURES wk some FTAS Fold – trace of synformal anticline axial plane

SFO undivided foliation -cleavage wk partly FTO Fold - trace of undivided axial plane

mod medium FTSA Fold – trace of antiformal syncline axial plane

SFS schistosity mod moderate FTSC Fold - trace of syncline axial plane

SFL laminations mod well developed FTSF Fold - trace of synform axial plane

SFC crenulation cleavage mod throughout FTSO Fold - trace of overturned syncline axial plane

SSC S-C fabric stg strong FV Fold - vergence towards antiform

SMY mylonite/mylonite zone int intense FVM Fold - m vergence

SHZ shear/ shear zone FVS Fold - s vergence

LIO linear fabric (constrictional or stretched features) unk finely FVZ Fold - z vergence

LIX lineation intersection(bed/clv, clv/clv) mod numerous IFA Dyke - aplite

LIM lineation mineral unk unknown IFGP Dyke - pegmatite

LIR lineation rodding IFO Dyke - felsic

LFA lineation of fold axis IFP Dyke - porphyry

LFM lineation of M vergent fold axis IMD Dyke - dolerite/diabase

LFZ lineation of Z vergent fold axis IOO Dyke - igneous

LFS lineation of S vergent fold axis JOO Joint - undivided

LGO Lineament - gravity

FOL folded lithologies LGW Lineament - gravity worms

FAA anticline LIM Lineation - mineral

FAS syncline LIO Lineation - undivided

FAP fold axial plane LIR Lineation - rodding

LIS Lineation - slickengrooves on fault surface

BRITTLE STRUCTURES LIX Lineation - intersection

ZFO fault LMO Lineament - magnetic

LMW Lineament - magnetic worms

ZFZ fault zone LTO Lineament – topographic

ZFR reverse fault SBO Primary surface - bedding

ZFN normal fault SBOO Primary surface - bedding overturned

ZFT thrust fault SCC Contact - interpretive caldera boundary

ZFS strike-slip fault SCD Contact - interpretive domain boundary

ZFG fault gouge/ clay/pug SCG Contact - interpretive gravity boundary

ZFL fault lineations (e.g:slickensides/slickenlines/slickenfibres/slips) SCI Contact - intrusive

ZFX fault breccia SCM Contact - interpretive magnetic boundary

ZFC cataclastic SCO Contact - undivided

SCS Contact - stratigraphic

ZRO fracture SCT Contact - interpretive terrane boundary

ZRZ fracture zone SCX Contact - outcrop boundary

JOO joints/ jointing SFB Primary surface - flow banding or cumulate banding

SFC Secondary surface - cleavage

SFCC Secondary surface - cleavage - crenulation

SFG Secondary surface - gneissosity

SFL Primary surface - laminations

SFO Secondary surface - foliation

SFS Secondary surface - schistosity

SFSC Secondary surface - schistosity - crenulation

SKB Secondary surface - kink band

STY Secondary surface - stylolite

SUA Unconformity - angular

SUD Unconformity - disconformity

SUN Unconformity - nonconformity

SUO Unconformity - undivided

TLC Trend line - geochemistry

TLM Trend line - magnetics

TLO Trend line - undivided

TLP Trend line - airphotos

YCH Younging - scour marks

YDEN Younging - density structures

YGB Younging - graded bedding

YNG Younging - undivided

YPIL Younging - pillows

YXB Younging - cross bedding

ZFC Fault - cataclastic

ZFD Fault - extensional detachment or low-angle normal fault

ZFG Fault - gouge / clay/ pug

ZFN Fault - normal

ZFO Fault - undivided

ZFQ Fault - oblique slip - undivided

ZFQDN Fault - oblique slip - dextral and normal - dextral transtension

ZFQDR Fault - oblique slip - dextral and reverse - dextral transpression

ZFQSN Fault - oblique slip - sinistral and normal - sinsitral transtension

ZFQSR Fault - oblique slip - sinistral and reverse - sinistral transpression

ZFR Fault - reverse

ZFS Fault - strike-slip - undivided

ZFSD Fault - strike-slip - dextral

ZFSS Fault - strike-slip - sinistral

ZFT Fault - thrust

ZFX Fault - breccia

ZMO Fault - mylonite zone

ZRO Fracture

ZSO Fault - shear

ZVC Vein - carbonate

ZVCA Vein - ankerite

ZVCF Vein - siderite

ZVCFA Vein - siderite - ankerite

ZVE Vein - epidote

ZVF Vein - limonite or ferruginous

ZVG Vein - gold-bearing

ZVK Vein - K-spar

ZVO Vein - undivided

ZVQ Vein - quartz

ZVS Vein - sulphide

GEOINFORMATICS REDTON ALTERATION ASSEMBLAGE CODES

Alt_type Alt_type_Description Alt_intensity Alt_style

style, distribution,

geometry

Alt_minerals

(AGSO codes) Alt_minerals_DescriptionAL Albitic ana anastomosing AB albite

AR Argillic, undivided ( ) *absolute % bd banded ACN acanthite

ARA Argillic, advanced tr trace (<2%) blb blebs ACT actinolite

ARI Argillic, intermediate wk weak (2-10%) box boxwork ADR andradite

ASS

Mineral Assemblage (name not

mentioned, but minerals given) mod

moderate/medium

(10-25%) ckd cockade ADS andesine

ASU acid sulphate stg strong (25-50%) cla clasts ADU adularia

BA Barite int intense (>50%) diss disseminated AEG aegirine

BLE Bleached fil fill AEN aenigmatite

BZ Biotization When Recoding legacy data ff fracture filling AG silver

BZMT biotite-magnetite wk (+/-) fld flooded AGL augelite

CD Chalcedonic wk minor frag fragments AGT aegirine-augite

CH Chloritization wk partly fram framboidal AIK aikinite

CN Carbonatization wk patchy fsel fracture selvage AK akermanite

CLAY clay alteration wk rare gran granular AKT aluminokataphorite

EZ Epidotization wk scattered hal halo/envelopes ALB alabandite

EZCH Epidote-chlorite wk some hybx hydrothermal breccia ALG allargentum

FD Felspathization unk unknown lam laminae ALM almandine

FN Fenitization len lenticular ALN allanite

FU Fuchsitic mass massive ALP allophane

GRA Graphitic mat matrix ALSI aluminosilicate (unspecified)

GS Greisen mot mottled ALT altaite

HM Hematization nod nodular ALU alunite

ILL illitic rep replacement/overprint AMB amblygonite

ILSM interlayered illite-smectite pat patches AMPH amphibole

JS Jasperoidal pod pod AMS amesite

KA Kaolinitic pv pervasive AN anorthite

KF K-feldspathization rcry recrystallised AND andalusite

KO Potassic rib ribbon ANG anglesite

MI Micaceous spo spotted ANH anhydrite

MNOX Manganese Oxide stain staining ANK ankerite

MT Magnetitic vsel vein selvage ANL analcime

NOT Not altered, fresh rock wrk wall-rock ANN annite

OX Oxidised ANR anorthoclase

PH Phyllic ANT anatase

PO Pyrrhotite unk no style mentioned AP apatite

PP Propylitic APO apophyllitePR Pyritic APY arsenopyrite

QAD quartz-adularia

QIL quartz-illite etc etc

QSK quartz-smectite-kaolinite

SK Skarn ZUN zunyite

SL Silicic/Silicification

SMEC smectite zone

SN Sinter

SO Sodic

SP Spilitisation

SR Sericitiziation

SRP Sericte-paragonite

SS Sausseritised

SU Sulphidic

SUB Sulphidic, Base Metals

SY Syenitized

SZ Serpentinization

TC Talc

TOUR Tourmalinisation

UND Altered (undifferentiated)

UNK Unknown

ZE Zeolitization

AGSO Minerals

Alt_minerals

(AGSO codes) Alt_minerals_Description

Alt_minerals


Alt_minerals


Alt_minerals


Alt_minerals


Alt_minerals


Alt_minerals


Alt_minerals


AB albite CFS clinoferrosilite FKT ferrikataphorite KDC kiddcreekite MSB moschellandsbergite PSC parascholzite SPL spinel VVT vivianite

ACN acanthite CHC chalcanthite FL fluorite KES kesterite MSC massicot PSG phosgenite SPN saponite WDG wodginite

ACT actinolite CHE chenevixite FLB freieslebenite KFS k-feldspar MSD magnesiosadanagite PSI psilomelane SPR sapphirine WDH woodhouseite

ADR andradite CHM chamosite FLL fluellite KLD kullerudite MSL mesolite PSM pseudomalachite SPS spessartine WFM wolframite

ADS andesine CHN chondrodite FLT florencite KLM kleemanite MST metastibnite PT platinum SPT spertiniite WHT whiteite

ADU adularia CHP chapmanite FMB ferrimolybdite KLN kaolinite MTB metatorbernite PTL petalite SPY sperrylite WKM wilkmanite

AEG aegirine CHQ clinoholmquistite FMT famatinite KLP kaliophilite MTC monticellite PTN plattnerite SRD serandite WLF wulfenite

AEN aenigmatite CHR chromite FO forsterite KLS kalsilite MTD matildite PTR potarite SRL schorl WLK wilkinsonite

AG silver CHS chalcostibite FPG ferropargasite KLY kellyite MTM muthmannite PTY platynite SRM schorlomite WLM willemite

AGL augelite CHT churchite FRB ferberite KMB kambaldaite MTR magnesiotaramite PTZ petzite SRT sartorite WLS willemseite

AGT aegirine-augite CHU clinohumite FRC ferrorichterite KMC kamacite MTT mangantantalite PVN pavonite SRZ strunzite WLY willyamite

AIK aikinite CIN cinnabar FRG fergusonite KNR knorringite MTY montroydite PWL powellite SSV stishovite WNC winchite

AK akermanite CKT cookite FRH frohbergite KPK krupkaite MUL mullite PXM pyroxmangite ST staurolite WNS wonesite

AKT aluminokataphorite CL chlorite FRK franklinite KR krennerite MWS mawsonite PY pyrite STA stibarsen WO wollastinite

ALB alabandite CLA clausthalite FS ferrosilite KRH kroehnkite MZC monazite-(ce) PYC pyrochroite STB stibnite WRD wardite

ALG allargentum CLAY clay mineral FSPD feldspathoid KRK kirkiite MZL monazite-(la) PYD polydymite STC stibiconite WRK wairakite

ALM almandine CLB columbite FTS ferrotschermakite KRM kuramite MZN monazite-(nd) PYG pyragyrite STD stannoidite WRT wurtzite

ALN allanite CLC chalcedony FTT ferrotantalite KRN kornerupine NAT natrite PYL pyrolusite STE stephanite WRU wairauite

ALP allophane CLD chloritoid FUC fuchsite KRS kaersutite NCL niccolite PYM pyromorphite STG strengite WSB weissbergite

ALSI aluminosilicate (unspecified) CLM calomel FWN ferrowinchite KRT krutaite NE nepheline PYOX oxidised pyrite STI stilleite WSH weishanite

ALT altaite CLN celsian FY fayalite KST kostovite NGL niggliite PYRX pyroxene STK stokesite WSS weissite

ALU alunite CLO chloanthite GARN garnierite KTK koutekite NI nickel PYS pyrosmalite STL stilbite WSV westerveldite

AMB amblygonite CLP chalcophanite GBM galenobismutite KTN kutnohorite NKD nukundamite QND qandilite STM sulphotsumoite WTC wittichenite

AMPH amphibole CLR coloradoite GBS gibbsite KTP katophorite NLG nullaginite QZ quartz STN stannite WTH witherite

AMS amesite CLS celestine GCX gorceixite KY kyanite NMN naumannite RAR ruarsite STP stilpnomelane WTT wittite

AN anorthite CNA chalconatronite GDL gadolinite KZL kozulite NRB norbergite RBK riebeckite STR strontianite WUS wustite

AND andalusite CNC conichalcite GED gedrite LAB labradorite NRN natron RBN robinsonite STS stistaite WVL wavellite

ANG anglesite CNL carnallite GEV geversite LBB liebenbergite NSB nisbite RCK rucklidgeite STT stichtite XEN xenotime

ANH anhydrite CNT carnotite GH gehlenite LCT leucite NSN nosean RCT richterite STU stutzite XNT xonotlite

ANK ankerite COAL coal GHN gahnite LFT laffittite NST norsethite RDH ramdohrite STV stevensite XTH xanthoconite

ANL analcime COB cobaltite GKL geikielite LGB lengenbachite NSU nsutite RDL rhodolite STW stillwaterite YGW yugawaralite

ANN annite COE coesite GL glass LLG loellingite NTA natroalunite RDN rhodonite STY stromeyerite YRW yarrowite

ANR anorthoclase COF coffinite GLB glauberite LMN limonite NTK nantokite RDS rhodochrosite STZ stolzite ZEOL zeolite

ANT anatase COL colemanite GLC glaucodot LMT laumontite NTN nontronite RE rhenium SUL sulphur ZKN zinkenite

AP apatite COR corundum GLN glaucophane LNG langisite NTR natrolite RH rhodium SULP sulphide ZNC zincite

APO apophyllite CPR cooperite GLT glauconite LNN linnaeite NYB nyboite RHN rhonite SVB svanbergite ZNOX oxidised zinc minerals

APY arsenopyrite CPT clinoptilolite GLX galaxite LOR lorandite OAMP orthoamphibole RIC rickardite SVN sulvanite ZNW zinnwaldite

AR Argillic CPX clinopyroxene GML gmelinite LPC lepidocrocite OCL orcelite RIO rutheniridosmine SWL stillwellite ZO zoisite

ARC aurichalcite CRB carrboydite GN galena LPD lepidolite OFR offretite RLG realgar SWT sweetite ZRK zirkelite

ARF arfvedsonite CRC crocoite GND gonnardite LPL lithiophilite OGC oligoclase RMB rammelsbergite SYL sylvite ZRN zircon

ARG aragonite CRD cordierite GNL greenalite LRN larnite OGN oregonite RMD ramsdellite SYN synchysite ZRT zaratiteARS arsenolite CRG chlorargyrite GNT garnet LRS larsenite OL olivine RMN romanechite TAE taenite ZUN zunyite

ART artinite CRK corkite GOS goslarite LRT laurite OLT olivenite RSP raspite TAN tellurantimony

AS arsenic CRL carrollite GP gypsum LRZ lorenzenite OME omeiite RSS rosasite TBM tellurobismuthite

ASOX oxidised arsenopyrite CRM cryptomelane GR graphite LTH lanthanite OMP omphacite RST rhodostannite TBR torbernite

AST aurostibite CRN carnegieite GRK greenockite LTP lithiophorite OPL opal RT rutile TCK tucekite

ATC atacamite CRO crossite GRS grossular LTT lautite OPQ opaque mineral RTA ruthenarsenite TDK todorokite

ATE atheneite CRR corrensite GRT groutite LVY levyne OPX orthopyroxene RTH rathite TE tellurium

ATG antigorite CRS cristobalite GRU grunerite LVZ lovozerite OR orthoclase RU ruthenium TELL tellurides

ATH anthophyllite CRT cerite GSD gersdorffite LWS lawsonite ORP orpiment RZN rozenite TGR tugarinovite

ATL antlerite CRV cervantite GSM gismondine LZ lizardite OS osmium SAL sodium alum TGS tungstite

ATN autunite CRY cryolite GSP gaspeite LZL lazulite OSA osarsite SANI sanidine TGT tungstenite

AU gold CSB costibite GT goethite LZN luzonite OSI osmiridium SAP strontium-apatite THN thenardite

AUG augite CSL cosalite GTM gatumbaite LZR lazurite OSM osumilite SAT sodium anthophyllite THR thorianite

AUS austinite CST cassiterite GUD gudmundite MAF magnesio-arfvedsonite OSZ osarizawite SAU sodium autunite THT thorite

AWR awaruite CTE cerianite GYZ goyazite MAK magnesio-aluminokataphorite OTM ottemannite SB antimony TIR tirodite

AX axinite CTG cuprotungstite HAP hydroxylapatite MAL malachite OTV otavite SBG sternbergite TLC talc

AZ azurite CTL chrysotile HBL hornblende MAT magnesio-anthophyllite OTW otwayite SBP stibiopalladinite TLM tulameenite

BBT babingtonite CTP catapleiite HBN hubnerite MAU meta-autunite PAR parisite SBV sobelevskite TLR tellurite

BCT boracite CU copper HBS hibschite MAX magnesio-axinite PAX paxite SBY sudburyite TLT teallite

BDL baddeleyite CUM cummingtonite HC hercynite MBD molybdite PB lead SCB sphaerocobaltite TLV tolovkite

BDT beudantite CUOX oxidised copper minerals HD hedenbergite MBL mirabilite PBA palladobismutharsenide SCH scheelite TMP thomsonite

BHM boehmite CUP cuprite HDA hydroxyapophyllite MBY montbrayite PBG plumbogummite SCL scolecite TNK talnakhite

BI bismuth CV covellite HDC hydrocerussite MC microcline PBJ plumbojarosite SCP scapolite TNL taeniolite

BKB brackebuschite CVK chevkinite HDL hidalgoite MCD magnesiochloritoid PBM plumbomicrolite SCR scorodite TNR tenorite

BLN berlinite CVT calaverite HDM hydromagnesite MCH magnesioclinoholmquistite PBOX oxidised lead minerals SCW scawtite TNT tennantite

BLT boulangerite CZO clinozoisite HDT hydrotungstite MCK mackinawite PBP plumbopalladinite SCZ scorzalite TOUR tourmaline

BMN bismuthinite DCK dickite HDY hedyphane MCM magnesiocummingtonite PCK pickeringite SD siderite TOZ topaz

BMT bismutite DCZ descloizite HDZ hydrozincite MCN metacinnabar PCL pyrochlore SDB serendibite TPH tephroite

BN bornite DFT duftite HED hedleyite MCS marcasite PCR pecoraite SDL sodalite TPL tapiolite

BNN bournonite DG digenite HEM hematite MCT moncheite PCT pectolite SDN sideronatrite TPY triphylite

BNS birnessite DI diopside HES hessite MDC madocite PD palladium SDO sudoite TR tremolite

BRA brannerite DMD diamond HL halite MDN mordenite PDA palladoarsenide SDP siderophyllite TRD tridymite

BRC brucite DNM dannemorite HLD hollandite MDR modderite PEN protoenstatite SDT studtite TRL trolleite

BRG barringtonite DOL dolomite HLR hellyerite MEI meionite PER periclase SE selenium TRM taramite

BRH brochantite DPT dioptase HLY halloysite MEL melilite PFE pumpellyite-fe2+ SEP sepiolite TRN trona

BRK brookite DRV dravite HMM hemimorphite MFD mansfieldite PFR playfairite SERI sericite TRO troilite

BRL beryl DSC dyscrasite HMQ holmquistite MFK magnesioferrikataphorite PG paragonite SERP serpentine TRP triplite

BRN braunite DSP diaspore HNG hingganite MGC magnesiochromite PGT pigeonite SFL safflorite TRQ turquoise

BRS barroisite DTL datolite HNT huntite MGD magnesiogedrite PHK phenakite SGD sodium gedrite TRV trevorite

BRT barite DVD davidite HOP hopeite MGF magnesioferrite PHL phlogopite SGL senegalite TS tschermakite

BRV bravoite DWS dawsonite HRM harmotome MGH maghemite PHOS phosphate SGN siegenite TSD trustedtite

BRX borax ECK eckermannite HS hastingsite MGN manganite PIL picro-ilmenite SHC shcherbakovite TSM tsumoite

BRY bromargyrite ED edenite HSD hinsdalite MGR mgriite PKN paakkonenite SHN shandite TTD tetradymite

BRZ berzelianite EDL eudialyte HSM hausmannite MGS magnesite PKO pekoite SHT shattuckite TTH tetrahedrite

BSM bismite ELB elbaite HTN huttonite MGT magnetite PL plagioclase SHZ scholzite TTL tantalite

BSN bastnaesite ELE electrum HTR halotrichite MGY miargyrite PLB polybasite SI silica TTN titanite

BST bustamite EMP emplectite HU humite MHB magnesiohornblende PLC pollucite SIL sillimanite TWN twinnite

BT biotite EN enstatite HUL heulandite MHQ magnesioholmquistite PLG palygorskite SKD sklodowskite TYL tyrrellite

BTF betafite ENG enargite HYL hyalophane MHS magnesiohastingsite PLI platiniridium SKN skinnerite U uranium

BTP breithauptite EP epidote HYN hauyne MICA mica PLL polylithionite SKT skutterudite UBG uytenbogaardtite

BTR bertrandite EPS epsomite HZL heazlewoodite MKT magnesiokataphorite PLN planerite SLA sellaite UMG umangite

BTW bytownite ERT erythrite IDA idaite MLD maldonite PLP phillipsite SLE saleeite UMN ullmannite

BXB bixbyite FAC ferro-actinolite IDG iodargyrite MLL millerite PLT platarsite SLG seligmannite UNK unknown

BZ Biotization FAN ferri-annite IGD ingodite MLN melonite PLV paolovite SLN selenite URC uranocircite

CA calcium FAP fluorapatite ILL illite MLR milarite PMG pumpellyite-mg SLR stellerite URE urea

CAL calcite FAT ferro-anthophyllite ILM ilmenite MLT melanterite PMN pumpellyite-mn SLV sylvanite URN uraninite

CAMP clino-amphibole FAY fluorapophyllite ILS ilsemannite MLY malayaite PMP pumpellyite SLW slawsonite UROX uranium oxide mineral

CAP chlorapatite FBG freibergite ILV ilvaite MMT mimetite PMT piemontite SMEC smectite URP uranophane

CARB carbonate FBR ferrobarroisite INE inesite MNC manganochromite PN pentlandite SMH smithite USP ulvospinel

CBE chrysoberyl FCH ferroclinoholmquistite IR iridium MNG meneghinite PO pyrrhotite SMK samarskite UV uvite

CBN cubanite FCL ferrocolumbite IRA iridarsenite MNOX manganese oxides PPH pyrophanite SMN smithsonite UVR uvarovite

CBZ chabazite FDR ferridravite IRO iridosmine MNS minnesotaite PPS phosphosiderite SMP stumpflite VAE vaesite

CC chalcocite FE iron IRS irarsite MNT montmorillonite PPU phosphuranylite SMR sanmartinite VEN veenite

CCH clinochlore FECB iron carbonate IXL ixiolite MNZ monazite PPY plumbopyrochlore SMS samsonite VES vesuvianite

CCL chrysocolla FED ferro-edenite JAR jarosite MOH mohite PQT pirquitasite SMT smaltite VIO violarite

CCN cancrinite FEK ferro-eckermannite JCB jacobsite MOL molybdenite PRC pearceite SMY semseyite VKG vikingite

CCP chalcopyrite FELD feldspar JD jadeite MOT mottramite PRG pargasite SN tin VLC vulcanite

CCS chalcosiderite FEMG ferromagnesian mineral JEP jeppeite MRB magnesioriebeckite PRH prehnite SND sanderite VLK velikite

CD Chalcedonic FEOX iron oxide JGF jugoldite-fe2+ MRC minrecordite PRL pyrophyllite SNG sanadagite VLM villamaninite

CDL crandallite FFT ferroferritschermakite JH johannsenite MRG margarite PRM pararammelsbergite SNJ seinajokite VLR valleriite

CDN caledonite FGD ferrogedrite JLP jalpaite MRK merenskyite PRP pyrope SNM senarmontite VLT valentinite

CDR calderite FGL ferroglaucophane JMS jamesonite MRL marialite PRR pararealgar SP sphalerite VND vanadinite

CEL celadonite FHB ferrohornblende JOS joseite MRS miersite PRS proustite SPC sopcheite VRM vermiculite

CEN clinoenstatite FHQ ferroholmquistite JRD jordanite MRW merwinite PRV perovskite SPD spodumene VRN vernaditeCER cerussite FKR ferrokaersutite JUN junoite MS muscovite PSB pseudobrookite SPH sodium phlogopite VRS variscite

GEOINFORMATICS REDTON LITHOLOGY CODES

INTRUSIVE lith code VOLCANIC lith code SEDIMENTS

lith

code METAMORPHIC

lith

code VOLCANICLASTIC

lith

code

ALTERED ROCKS

(original rock type unidentifiable)

lith

code OTHER

lith

code

Undifferentiated Intrusives IOO Undifferentiated Volcanic Rocks VOO Undifferentiated Sediments SOO Undifferentiated metamorphic rock XOO Undifferentiated Volcaniclastic Rocks YOO Altered Rock, Undivided AOO Unknown rock type OOO

porphyry, undiff. IOP Undifferentiated Volcanic Rocks - porphyritic VOP Conglomerate SCO Amphibolite, undivided XAO tuff - unknown composition YOT Altered intrusive rock AIO Unknown, missing interval, lost sample OMIUndifferentiated Felsic Intrusives IFO Undifferentiated Felsic Volcanic Rocks VFO Conglomerate - boulder SCB Gneiss, undivided XGO agglomerate - unknown composition YOA Altered volcanic rock AVO Unknown, not logged ONLPorphyritic felsic intrusive IFP Undifferentiated Felsic Volcanic Rocks - porphyritic VFP Conglomerate - pebble/cobble SCC granulite XGG ignimbrite - unknown composition YOI Altered sedimentary rock ASS Drill Casing CASE

Pegmatite, undivided IFPG Rhyolite VFR Conglomerate - granule SCG Ortho-gneiss XGI Undiff Felsic Volcaniclastics YFO Albite altered rock AAO

Granite IFG Rhyolite - quartz +/- feldspar phyric VFRP Conglomerate - polymictic SCP Migmatite XGM agglomerate felsic YFA Biotite alteration ABO SURFICIAL

Porphyritic granite IFGP Dacite VFD Conglomerate - monomictic SCM quartzofeldspathic gneiss XGQ ignimbrite - felsic YFI Carbonate-chlorite ACH Overburden OVER

adamellite IFGA Dacite - quartz +/- feldspar phyric VFDP Sedimentary Breccia (sharpstone Conglom.) SCX Para-gneiss XGS tuff - felsic YFT Carbonate altered rock ACO undivided regolith ROO

albite granite IFGB Rhyodacite VFRD clastic sediments (coarser than siltsize) SSO pelitic gneiss XGSP Rhyolite tuff YFR Fuchsite alteration AFO soil ROS

aplite IFA Undifferentiated Intermediate Volcanic Rocks VIO Sandstone/Arenite SSA psammitic gneiss XGSS Dacite tuff YFD Chloritic alteration AHO undivided residual regolith RRO

charnockite IFC Intermediate Volcanics - quartz +/- feldspar phyric VIOP Calcareous arenite/sandstone SSB eclogite XEO Undiff Intermediate Volcaniclastics YIO K-spar alteration AKO Transported colluvium RTC

Granodiorite IFD Intermediate Volcanics - vesicular/amygdaloidal VIOV Carbonaceous arenite/sandstone SSC Hornfels, undivided XHO agglomerate - intermediate YIA Silica-carbonate AQC undivided transported regolith RTO

Porphyritic granodiorite IFDP Andesite VIA Sulphidic arenite/sandstone SSZ dolomitic marble XLD ignimbrite - intermediate YII Silica-sericite AQE Unconsolidated alluvium RTA

Trondjhemite IFJ Andesite - quartz +/- feldspar phyric VIAP Arkose SSK marble XLO tuff - intermediate YIT Silica-fuchsite AQF gravel RTG

Tonalite IFT Andesite - amygdaloidal/vesicular VIAV Volcanic arenite/sandstone SSV Schist, undivided XSO andesite tuff YIAT Silica-chlorite AQH till RTT

Alkalic Intrusion, undivided IKO basaltic andesite VIB Quartzite SSQ Phyllite/slate, undivided XPO Undiff Mafic Volcaniclastics YMO Silica alteration AQO Gossan RGO

Syenite IKS trachyandesite VIT Wacke SWO Biotite schist XSB agglomerate - mafic YMA Sericite-Carbonate ASC FAULT ZONES

Porphyritic syenite IKSP Alkalic volcanic, undivided VKO Calcareous Greywacke SWB carbonate schist and calc-schist XSC ignimbrite - mafic YMI Sericitic alteration ASO Fault/Fault zone ZFO

nepheline syenite IKSN Alkalic volcanic - quartz +/- feldspar phyric VKOP Carbonaceous/graphitic Greywacke SWC feldspathic schist XSF tuff - mafic YMT Sericite-chlorite ASH fault gouge ZFG

quartz syenite IKSQ Latite (porphyritic) VKL Sulphidic Greywacke SWZ schist - graphitic XSG Sericite-clay ASL fault breccia ZFX

Albitite IKA alkali feldspar rhyolite VKR Siltstone SIO Chlorite schist XSH Clay alteration ALO Mylonite/tectonite ZMO

Carbonatite IKC Trachyte VKT Calcareous siltstone SIB sericite schist XSK Clay-chlorite ALH

alkali feldspar granite / syenogranite IKGF Undifferentiated Mafic Volcanic Rocks VMO Carbonaceous/graphitic siltstone SIC muscovite schist XSM Dominantly sulphide rock AZO VEINS

Shoshonite IKH Mafic lava; amygdaloidal/vesicular VMOV Quartzose/siliceous siltstone SIQ pelitic schist XSP vein, undifferentiated ZVOUndifferentiated Intermediate Intrusives IIO Basalt VMB Sulphidic siltstone SIZ psammitic schist XSS carbonate-dominant vein ZVCPorphyritic intermediate intrusive IIP Basalt - amygdaloidal/vesicular VMBV Argillite SAO Psammite, undivided XMO quartz-dominant vein ZVQ

Diorite IID Pillow basalt VMBP Calcareous argillite/shale/mudstone SAB meta-quartzite XQO quartz-carbonate dominant vein ZVQC

Porphyritic diorite intrusive IIDP olivine basalt VMBO Carbonaceous/graphitic argillite/shale/mudstone SAC Talc - Chlorite schist XST quartz-feldspar dominant vein ZVQF

Monzonite IIM Tholeitic basalt VMBT Quartzose/siliceous argillite SAQ meta-ultramafic undivided XUO sulphidic vein ZVS

Porphyritic monzonite intrusive IIMP komatiitic basalt VMK Sulphidic argillite/shale/mudstone SAZ serpentinite XUS

Quartz diorite IIQ Undifferentiated Ultramafic Volcanic Rocks VUO shale SIH

Porphyritic quartz diorite intrusive IIQP Komatiite VUK mudstone SIM

Quartz monzonite IIZ Peridotite VUP Chert STO

Porphyritic quartz monzonite intrusive IIZP Pyroxenite VUX Banded Iron Formation STF

Monzodiorite III sulphidic chert STZ

Porphyritic monzodiorite intrusive IIIP Carbonate sediments, undivided SLO

Undifferentiated Mafic Intrusives IMO Limestone SLL

Porphyritic mafic intrusive IMP Dolomite/Dolostone SLD

Gabbro IMG Biogenic rock, undifferentiated BOO

hornblende gabbro IMGH Biogenic carbonaceous deposit, undiff BCO

gabbronorite IMGN

olivine gabbro IMGO

Norite IMN

Troctolite IMT

Dolerite / Diabase IMD

Undifferentiated Ultramafic Intrusion IUO

Peridotite IUP

Picrite IUR

Pyroxenite IUX

clinopyroxenite IUXC

orthopyroxenite IUXO

Dunite IUD

Hornblendite IUH

Harzburgite IUZ

Undifferentiated lamprophyre ILO

GEOINFORMATICS REDTON VEINING CODES

Vein_style Vein_intensity Vein_mineral

Code

includes: style-geometry-

structure-size code code

use same code

abbreviation as for AGSO

minerals

BND Boudinaged Vein ( ) *absolute % UNK unknown

BRX Vein Breccia tr trace (<2%)

CKD Cockade Vein wk weak (2-10%) ACN acanthite

COL Colloform Vein mod moderate/medium (10-25%) ACT actinolite

CON Conjugate Veins stg strong (25-50%) ADU adularia

CRC Crackle Vein int intense (>50%) AEG aegirine

DRU Drusy unk unknown intensity AGT aegirine-augite

EEN En Echelon Veins AEN aenigmatite

EXT Extensional Vein When Recoding legacy data AIK aikinite

FELD Narrow felsic dyke/vein wk few AK akermanite

FMV Fine/micro-veins wk minor ALB alabandite

FOL Folded vein wk (+/-) AB albite

FRV Fracture Veins wk some ALN allanite

FTV Fault-related veins wk partly ALG allargentum

HLN Hairline Veins wk rare ALP allophane

INTD Narow intermediate dyke/vein wk scattered ALM almandine

IRR Irregular / undeformed / segmented wk patchy ALT altaite

LAC Laced veinlets wk irregular AKT aluminokataphorite

LAM Laminated Veins ALSI aluminosilicate (unspecified)

LAMD Narrow lamprophyre dyke/vein mod common ALU alunite

LIND Late intrusive dyke/stringer vein mod numerous AMB amblygonite

MAS Massive Veins mod many AMS amesite

NET Net-like veining mod regular AMPH amphibole

PEG Pegmatite Veins etc etc etc etc

PLN Planar Veins

PTY Ptygmatic folded veins

RIB Ribbon Veins

SHR Sheared Veins

SHT Sheeted Veins

SIG Sigmoidal Veins

SMS Seams

STK Stockwork Veins

STR Stringer Veins

STY Stylolitic

SYND Narrow syenitic dyke/vein

TEN Tension Gashes

UND Undifferentiated Veins / veinlets

WSP Wispy

GEOINFORMATICS REDTON STRUCTURE CODES

Drilling / hand specimen Data Mapping Data

CODE STRUCTURE_1 INTENSITY CODE DESCRIPTION

PRIMARY STRUCTURES FAA Fold axis - anticline

MAS massive undeformed tr trace FAAF Fold axis - antiform

SBO bedding / bedded wk weak FAAO Fold axis - overturned anticline

SBOO bedding overturned mod moderate/medium FAO Fold axis - undivided

SFB Primary surface - flow banding or cumulate banding stg strong FAP Fold - axial plane

YCH Younging - scour marks int intense FAS Fold axis - syncline

YDEN Younging - density structures unk unknown intensity FASF Fold axis - synform

YGB Younging - graded bedding FASO Fold axis - overturned syncline

YNG Younging - undivided When Recoding legacy data FFA Fold axis - undivided

YPIL Younging - pillows wk weak FTAC Fold - trace of anticline axial plane

YXB Younging - cross bedding wk poorly FTAF Fold - trace of antiform axial plane

wk (+/-) FTAO Fold - trace of overturned anticline axial plane

DUCTILE STRUCTURES wk some FTAS Fold – trace of synformal anticline axial plane

SFO undivided foliation -cleavage wk partly FTO Fold - trace of undivided axial plane

mod medium FTSA Fold – trace of antiformal syncline axial plane

SFS schistosity mod moderate FTSC Fold - trace of syncline axial plane

SFL laminations mod well developed FTSF Fold - trace of synform axial plane

SFC crenulation cleavage mod throughout FTSO Fold - trace of overturned syncline axial plane

SSC S-C fabric stg strong FV Fold - vergence towards antiform

SMY mylonite/mylonite zone int intense FVM Fold - m vergence

SHZ shear/ shear zone FVS Fold - s vergence

LIO linear fabric (constrictional or stretched features) unk finely FVZ Fold - z vergence

LIX lineation intersection(bed/clv, clv/clv) mod numerous IFA Dyke - aplite

LIM lineation mineral unk unknown IFGP Dyke - pegmatite

LIR lineation rodding IFO Dyke - felsic

LFA lineation of fold axis IFP Dyke - porphyry

LFM lineation of M vergent fold axis IMD Dyke - dolerite/diabase

LFZ lineation of Z vergent fold axis IOO Dyke - igneous

LFS lineation of S vergent fold axis JOO Joint - undivided

LGO Lineament - gravity

FOL folded lithologies LGW Lineament - gravity worms

FAA anticline LIM Lineation - mineral

FAS syncline LIO Lineation - undivided

FAP fold axial plane LIR Lineation - rodding

LIS Lineation - slickengrooves on fault surface

BRITTLE STRUCTURES LIX Lineation - intersection

ZFO fault LMO Lineament - magnetic

LMW Lineament - magnetic worms

ZFZ fault zone LTO Lineament – topographic

ZFR reverse fault SBO Primary surface - bedding

ZFN normal fault SBOO Primary surface - bedding overturned

ZFT thrust fault SCC Contact - interpretive caldera boundary

ZFS strike-slip fault SCD Contact - interpretive domain boundary

ZFG fault gouge/ clay/pug SCG Contact - interpretive gravity boundary

ZFL fault lineations (e.g:slickensides/slickenlines/slickenfibres/slips) SCI Contact - intrusive

ZFX fault breccia SCM Contact - interpretive magnetic boundary

ZFC cataclastic SCO Contact - undivided

SCS Contact - stratigraphic

ZRO fracture SCT Contact - interpretive terrane boundary

ZRZ fracture zone SCX Contact - outcrop boundary

JOO joints/ jointing SFB Primary surface - flow banding or cumulate banding

SFC Secondary surface - cleavage

SFCC Secondary surface - cleavage - crenulation

SFG Secondary surface - gneissosity

SFL Primary surface - laminations

SFO Secondary surface - foliation

SFS Secondary surface - schistosity

SFSC Secondary surface - schistosity - crenulation

SKB Secondary surface - kink band

STY Secondary surface - stylolite

SUA Unconformity - angular

SUD Unconformity - disconformity

SUN Unconformity - nonconformity

SUO Unconformity - undivided

TLC Trend line - geochemistry

TLM Trend line - magnetics

TLO Trend line - undivided

TLP Trend line - airphotos

YCH Younging - scour marks

YDEN Younging - density structures

YGB Younging - graded bedding

YNG Younging - undivided

YPIL Younging - pillows

YXB Younging - cross bedding

ZFC Fault - cataclastic

ZFD Fault - extensional detachment or low-angle normal fault

ZFG Fault - gouge / clay/ pug

ZFN Fault - normal

ZFO Fault - undivided

ZFQ Fault - oblique slip - undivided

ZFQDN Fault - oblique slip - dextral and normal - dextral transtension

ZFQDR Fault - oblique slip - dextral and reverse - dextral transpression

ZFQSN Fault - oblique slip - sinistral and normal - sinsitral transtension

ZFQSR Fault - oblique slip - sinistral and reverse - sinistral transpression

ZFR Fault - reverse

ZFS Fault - strike-slip - undivided

ZFSD Fault - strike-slip - dextral

ZFSS Fault - strike-slip - sinistral

ZFT Fault - thrust

ZFX Fault - breccia

ZMO Fault - mylonite zone

ZRO Fracture

ZSO Fault - shear

ZVC Vein - carbonate

ZVCA Vein - ankerite

ZVCF Vein - siderite

ZVCFA Vein - siderite - ankerite

ZVE Vein - epidote

ZVF Vein - limonite or ferruginous

ZVG Vein - gold-bearing

ZVK Vein - K-spar

ZVO Vein - undivided

ZVQ Vein - quartz

ZVS Vein - sulphide

GEOINFORMATICS REDTON ALTERATION ASSEMBLAGE CODES

Alt_type Alt_type_Description Alt_intensity Alt_style

style, distribution,

geometry

Alt_minerals

(AGSO codes) Alt_minerals_DescriptionAL Albitic ana anastomosing AB albite

AR Argillic, undivided ( ) *absolute % bd banded ACN acanthite

ARA Argillic, advanced tr trace (<2%) blb blebs ACT actinolite

ARI Argillic, intermediate wk weak (2-10%) box boxwork ADR andradite

ASS

Mineral Assemblage (name not

mentioned, but minerals given) mod

moderate/medium

(10-25%) ckd cockade ADS andesine

ASU acid sulphate stg strong (25-50%) cla clasts ADU adularia

BA Barite int intense (>50%) diss disseminated AEG aegirine

BLE Bleached fil fill AEN aenigmatite

BZ Biotization When Recoding legacy data ff fracture filling AG silver

BZMT biotite-magnetite wk (+/-) fld flooded AGL augelite

CD Chalcedonic wk minor frag fragments AGT aegirine-augite

CH Chloritization wk partly fram framboidal AIK aikinite

CN Carbonatization wk patchy fsel fracture selvage AK akermanite

CLAY clay alteration wk rare gran granular AKT aluminokataphorite

EZ Epidotization wk scattered hal halo/envelopes ALB alabandite

EZCH Epidote-chlorite wk some hybx hydrothermal breccia ALG allargentum

FD Felspathization unk unknown lam laminae ALM almandine

FN Fenitization len lenticular ALN allanite

FU Fuchsitic mass massive ALP allophane

GRA Graphitic mat matrix ALSI aluminosilicate (unspecified)

GS Greisen mot mottled ALT altaite

HM Hematization nod nodular ALU alunite

ILL illitic rep replacement/overprint AMB amblygonite

ILSM interlayered illite-smectite pat patches AMPH amphibole

JS Jasperoidal pod pod AMS amesite

KA Kaolinitic pv pervasive AN anorthite

KF K-feldspathization rcry recrystallised AND andalusite

KO Potassic rib ribbon ANG anglesite

MI Micaceous spo spotted ANH anhydrite

MNOX Manganese Oxide stain staining ANK ankerite

MT Magnetitic vsel vein selvage ANL analcime

NOT Not altered, fresh rock wrk wall-rock ANN annite

OX Oxidised ANR anorthoclase

PH Phyllic ANT anatase

PO Pyrrhotite unk no style mentioned AP apatite

PP Propylitic APO apophyllitePR Pyritic APY arsenopyrite

QAD quartz-adularia

QIL quartz-illite etc etc

QSK quartz-smectite-kaolinite

SK Skarn ZUN zunyite

SL Silicic/Silicification

SMEC smectite zone

SN Sinter

SO Sodic

SP Spilitisation

SR Sericitiziation

SRP Sericte-paragonite

SS Sausseritised

SU Sulphidic

SUB Sulphidic, Base Metals

SY Syenitized

SZ Serpentinization

TC Talc

TOUR Tourmalinisation

UND Altered (undifferentiated)

UNK Unknown

ZE Zeolitization

AGSO Minerals

Alt_minerals


Alt_minerals


Alt_minerals


Alt_minerals


Alt_minerals


Alt_minerals


Alt_minerals


Alt_minerals


AB albite CFS clinoferrosilite FKT ferrikataphorite KDC kiddcreekite MSB moschellandsbergite PSC parascholzite SPL spinel VVT vivianite

ACN acanthite CHC chalcanthite FL fluorite KES kesterite MSC massicot PSG phosgenite SPN saponite WDG wodginite

ACT actinolite CHE chenevixite FLB freieslebenite KFS k-feldspar MSD magnesiosadanagite PSI psilomelane SPR sapphirine WDH woodhouseite

ADR andradite CHM chamosite FLL fluellite KLD kullerudite MSL mesolite PSM pseudomalachite SPS spessartine WFM wolframite

ADS andesine CHN chondrodite FLT florencite KLM kleemanite MST metastibnite PT platinum SPT spertiniite WHT whiteite

ADU adularia CHP chapmanite FMB ferrimolybdite KLN kaolinite MTB metatorbernite PTL petalite SPY sperrylite WKM wilkmanite

AEG aegirine CHQ clinoholmquistite FMT famatinite KLP kaliophilite MTC monticellite PTN plattnerite SRD serandite WLF wulfenite

AEN aenigmatite CHR chromite FO forsterite KLS kalsilite MTD matildite PTR potarite SRL schorl WLK wilkinsonite

AG silver CHS chalcostibite FPG ferropargasite KLY kellyite MTM muthmannite PTY platynite SRM schorlomite WLM willemite

AGL augelite CHT churchite FRB ferberite KMB kambaldaite MTR magnesiotaramite PTZ petzite SRT sartorite WLS willemseite

AGT aegirine-augite CHU clinohumite FRC ferrorichterite KMC kamacite MTT mangantantalite PVN pavonite SRZ strunzite WLY willyamite

AIK aikinite CIN cinnabar FRG fergusonite KNR knorringite MTY montroydite PWL powellite SSV stishovite WNC winchite

AK akermanite CKT cookite FRH frohbergite KPK krupkaite MUL mullite PXM pyroxmangite ST staurolite WNS wonesite

AKT aluminokataphorite CL chlorite FRK franklinite KR krennerite MWS mawsonite PY pyrite STA stibarsen WO wollastinite

ALB alabandite CLA clausthalite FS ferrosilite KRH kroehnkite MZC monazite-(ce) PYC pyrochroite STB stibnite WRD wardite

ALG allargentum CLAY clay mineral FSPD feldspathoid KRK kirkiite MZL monazite-(la) PYD polydymite STC stibiconite WRK wairakite

ALM almandine CLB columbite FTS ferrotschermakite KRM kuramite MZN monazite-(nd) PYG pyragyrite STD stannoidite WRT wurtzite

ALN allanite CLC chalcedony FTT ferrotantalite KRN kornerupine NAT natrite PYL pyrolusite STE stephanite WRU wairauite

ALP allophane CLD chloritoid FUC fuchsite KRS kaersutite NCL niccolite PYM pyromorphite STG strengite WSB weissbergite

ALSI aluminosilicate (unspecified) CLM calomel FWN ferrowinchite KRT krutaite NE nepheline PYOX oxidised pyrite STI stilleite WSH weishanite

ALT altaite CLN celsian FY fayalite KST kostovite NGL niggliite PYRX pyroxene STK stokesite WSS weissite

ALU alunite CLO chloanthite GARN garnierite KTK koutekite NI nickel PYS pyrosmalite STL stilbite WSV westerveldite

AMB amblygonite CLP chalcophanite GBM galenobismutite KTN kutnohorite NKD nukundamite QND qandilite STM sulphotsumoite WTC wittichenite

AMPH amphibole CLR coloradoite GBS gibbsite KTP katophorite NLG nullaginite QZ quartz STN stannite WTH witherite

AMS amesite CLS celestine GCX gorceixite KY kyanite NMN naumannite RAR ruarsite STP stilpnomelane WTT wittite

AN anorthite CNA chalconatronite GDL gadolinite KZL kozulite NRB norbergite RBK riebeckite STR strontianite WUS wustite

AND andalusite CNC conichalcite GED gedrite LAB labradorite NRN natron RBN robinsonite STS stistaite WVL wavellite

ANG anglesite CNL carnallite GEV geversite LBB liebenbergite NSB nisbite RCK rucklidgeite STT stichtite XEN xenotime

ANH anhydrite CNT carnotite GH gehlenite LCT leucite NSN nosean RCT richterite STU stutzite XNT xonotlite

ANK ankerite COAL coal GHN gahnite LFT laffittite NST norsethite RDH ramdohrite STV stevensite XTH xanthoconite

ANL analcime COB cobaltite GKL geikielite LGB lengenbachite NSU nsutite RDL rhodolite STW stillwaterite YGW yugawaralite

ANN annite COE coesite GL glass LLG loellingite NTA natroalunite RDN rhodonite STY stromeyerite YRW yarrowite

ANR anorthoclase COF coffinite GLB glauberite LMN limonite NTK nantokite RDS rhodochrosite STZ stolzite ZEOL zeolite

ANT anatase COL colemanite GLC glaucodot LMT laumontite NTN nontronite RE rhenium SUL sulphur ZKN zinkenite

AP apatite COR corundum GLN glaucophane LNG langisite NTR natrolite RH rhodium SULP sulphide ZNC zincite

APO apophyllite CPR cooperite GLT glauconite LNN linnaeite NYB nyboite RHN rhonite SVB svanbergite ZNOX oxidised zinc minerals

APY arsenopyrite CPT clinoptilolite GLX galaxite LOR lorandite OAMP orthoamphibole RIC rickardite SVN sulvanite ZNW zinnwaldite

AR Argillic CPX clinopyroxene GML gmelinite LPC lepidocrocite OCL orcelite RIO rutheniridosmine SWL stillwellite ZO zoisite

ARC aurichalcite CRB carrboydite GN galena LPD lepidolite OFR offretite RLG realgar SWT sweetite ZRK zirkelite

ARF arfvedsonite CRC crocoite GND gonnardite LPL lithiophilite OGC oligoclase RMB rammelsbergite SYL sylvite ZRN zircon

ARG aragonite CRD cordierite GNL greenalite LRN larnite OGN oregonite RMD ramsdellite SYN synchysite ZRT zaratiteARS arsenolite CRG chlorargyrite GNT garnet LRS larsenite OL olivine RMN romanechite TAE taenite ZUN zunyite

ART artinite CRK corkite GOS goslarite LRT laurite OLT olivenite RSP raspite TAN tellurantimony

AS arsenic CRL carrollite GP gypsum LRZ lorenzenite OME omeiite RSS rosasite TBM tellurobismuthite

ASOX oxidised arsenopyrite CRM cryptomelane GR graphite LTH lanthanite OMP omphacite RST rhodostannite TBR torbernite

AST aurostibite CRN carnegieite GRK greenockite LTP lithiophorite OPL opal RT rutile TCK tucekite

ATC atacamite CRO crossite GRS grossular LTT lautite OPQ opaque mineral RTA ruthenarsenite TDK todorokite

ATE atheneite CRR corrensite GRT groutite LVY levyne OPX orthopyroxene RTH rathite TE tellurium

ATG antigorite CRS cristobalite GRU grunerite LVZ lovozerite OR orthoclase RU ruthenium TELL tellurides

ATH anthophyllite CRT cerite GSD gersdorffite LWS lawsonite ORP orpiment RZN rozenite TGR tugarinovite

ATL antlerite CRV cervantite GSM gismondine LZ lizardite OS osmium SAL sodium alum TGS tungstite

ATN autunite CRY cryolite GSP gaspeite LZL lazulite OSA osarsite SANI sanidine TGT tungstenite

AU gold CSB costibite GT goethite LZN luzonite OSI osmiridium SAP strontium-apatite THN thenardite

AUG augite CSL cosalite GTM gatumbaite LZR lazurite OSM osumilite SAT sodium anthophyllite THR thorianite

AUS austinite CST cassiterite GUD gudmundite MAF magnesio-arfvedsonite OSZ osarizawite SAU sodium autunite THT thorite

AWR awaruite CTE cerianite GYZ goyazite MAK magnesio-aluminokataphorite OTM ottemannite SB antimony TIR tirodite

AX axinite CTG cuprotungstite HAP hydroxylapatite MAL malachite OTV otavite SBG sternbergite TLC talc

AZ azurite CTL chrysotile HBL hornblende MAT magnesio-anthophyllite OTW otwayite SBP stibiopalladinite TLM tulameenite

BBT babingtonite CTP catapleiite HBN hubnerite MAU meta-autunite PAR parisite SBV sobelevskite TLR tellurite

BCT boracite CU copper HBS hibschite MAX magnesio-axinite PAX paxite SBY sudburyite TLT teallite

BDL baddeleyite CUM cummingtonite HC hercynite MBD molybdite PB lead SCB sphaerocobaltite TLV tolovkite

BDT beudantite CUOX oxidised copper minerals HD hedenbergite MBL mirabilite PBA palladobismutharsenide SCH scheelite TMP thomsonite

BHM boehmite CUP cuprite HDA hydroxyapophyllite MBY montbrayite PBG plumbogummite SCL scolecite TNK talnakhite

BI bismuth CV covellite HDC hydrocerussite MC microcline PBJ plumbojarosite SCP scapolite TNL taeniolite

BKB brackebuschite CVK chevkinite HDL hidalgoite MCD magnesiochloritoid PBM plumbomicrolite SCR scorodite TNR tenorite

BLN berlinite CVT calaverite HDM hydromagnesite MCH magnesioclinoholmquistite PBOX oxidised lead minerals SCW scawtite TNT tennantite

BLT boulangerite CZO clinozoisite HDT hydrotungstite MCK mackinawite PBP plumbopalladinite SCZ scorzalite TOUR tourmaline

BMN bismuthinite DCK dickite HDY hedyphane MCM magnesiocummingtonite PCK pickeringite SD siderite TOZ topaz

BMT bismutite DCZ descloizite HDZ hydrozincite MCN metacinnabar PCL pyrochlore SDB serendibite TPH tephroite

BN bornite DFT duftite HED hedleyite MCS marcasite PCR pecoraite SDL sodalite TPL tapiolite

BNN bournonite DG digenite HEM hematite MCT moncheite PCT pectolite SDN sideronatrite TPY triphylite

BNS birnessite DI diopside HES hessite MDC madocite PD palladium SDO sudoite TR tremolite

BRA brannerite DMD diamond HL halite MDN mordenite PDA palladoarsenide SDP siderophyllite TRD tridymite

BRC brucite DNM dannemorite HLD hollandite MDR modderite PEN protoenstatite SDT studtite TRL trolleite

BRG barringtonite DOL dolomite HLR hellyerite MEI meionite PER periclase SE selenium TRM taramite

BRH brochantite DPT dioptase HLY halloysite MEL melilite PFE pumpellyite-fe2+ SEP sepiolite TRN trona

BRK brookite DRV dravite HMM hemimorphite MFD mansfieldite PFR playfairite SERI sericite TRO troilite

BRL beryl DSC dyscrasite HMQ holmquistite MFK magnesioferrikataphorite PG paragonite SERP serpentine TRP triplite

BRN braunite DSP diaspore HNG hingganite MGC magnesiochromite PGT pigeonite SFL safflorite TRQ turquoise

BRS barroisite DTL datolite HNT huntite MGD magnesiogedrite PHK phenakite SGD sodium gedrite TRV trevorite

BRT barite DVD davidite HOP hopeite MGF magnesioferrite PHL phlogopite SGL senegalite TS tschermakite

BRV bravoite DWS dawsonite HRM harmotome MGH maghemite PHOS phosphate SGN siegenite TSD trustedtite

BRX borax ECK eckermannite HS hastingsite MGN manganite PIL picro-ilmenite SHC shcherbakovite TSM tsumoite

BRY bromargyrite ED edenite HSD hinsdalite MGR mgriite PKN paakkonenite SHN shandite TTD tetradymite

BRZ berzelianite EDL eudialyte HSM hausmannite MGS magnesite PKO pekoite SHT shattuckite TTH tetrahedrite

BSM bismite ELB elbaite HTN huttonite MGT magnetite PL plagioclase SHZ scholzite TTL tantalite

BSN bastnaesite ELE electrum HTR halotrichite MGY miargyrite PLB polybasite SI silica TTN titanite

BST bustamite EMP emplectite HU humite MHB magnesiohornblende PLC pollucite SIL sillimanite TWN twinnite

BT biotite EN enstatite HUL heulandite MHQ magnesioholmquistite PLG palygorskite SKD sklodowskite TYL tyrrellite

BTF betafite ENG enargite HYL hyalophane MHS magnesiohastingsite PLI platiniridium SKN skinnerite U uranium

BTP breithauptite EP epidote HYN hauyne MICA mica PLL polylithionite SKT skutterudite UBG uytenbogaardtite

BTR bertrandite EPS epsomite HZL heazlewoodite MKT magnesiokataphorite PLN planerite SLA sellaite UMG umangite

BTW bytownite ERT erythrite IDA idaite MLD maldonite PLP phillipsite SLE saleeite UMN ullmannite

BXB bixbyite FAC ferro-actinolite IDG iodargyrite MLL millerite PLT platarsite SLG seligmannite UNK unknown

BZ Biotization FAN ferri-annite IGD ingodite MLN melonite PLV paolovite SLN selenite URC uranocircite

CA calcium FAP fluorapatite ILL illite MLR milarite PMG pumpellyite-mg SLR stellerite URE urea

CAL calcite FAT ferro-anthophyllite ILM ilmenite MLT melanterite PMN pumpellyite-mn SLV sylvanite URN uraninite

CAMP clino-amphibole FAY fluorapophyllite ILS ilsemannite MLY malayaite PMP pumpellyite SLW slawsonite UROX uranium oxide mineral

CAP chlorapatite FBG freibergite ILV ilvaite MMT mimetite PMT piemontite SMEC smectite URP uranophane

CARB carbonate FBR ferrobarroisite INE inesite MNC manganochromite PN pentlandite SMH smithite USP ulvospinel

CBE chrysoberyl FCH ferroclinoholmquistite IR iridium MNG meneghinite PO pyrrhotite SMK samarskite UV uvite

CBN cubanite FCL ferrocolumbite IRA iridarsenite MNOX manganese oxides PPH pyrophanite SMN smithsonite UVR uvarovite

CBZ chabazite FDR ferridravite IRO iridosmine MNS minnesotaite PPS phosphosiderite SMP stumpflite VAE vaesite

CC chalcocite FE iron IRS irarsite MNT montmorillonite PPU phosphuranylite SMR sanmartinite VEN veenite

CCH clinochlore FECB iron carbonate IXL ixiolite MNZ monazite PPY plumbopyrochlore SMS samsonite VES vesuvianite

CCL chrysocolla FED ferro-edenite JAR jarosite MOH mohite PQT pirquitasite SMT smaltite VIO violarite

CCN cancrinite FEK ferro-eckermannite JCB jacobsite MOL molybdenite PRC pearceite SMY semseyite VKG vikingite

CCP chalcopyrite FELD feldspar JD jadeite MOT mottramite PRG pargasite SN tin VLC vulcanite

CCS chalcosiderite FEMG ferromagnesian mineral JEP jeppeite MRB magnesioriebeckite PRH prehnite SND sanderite VLK velikite

CD Chalcedonic FEOX iron oxide JGF jugoldite-fe2+ MRC minrecordite PRL pyrophyllite SNG sanadagite VLM villamaninite

CDL crandallite FFT ferroferritschermakite JH johannsenite MRG margarite PRM pararammelsbergite SNJ seinajokite VLR valleriite

CDN caledonite FGD ferrogedrite JLP jalpaite MRK merenskyite PRP pyrope SNM senarmontite VLT valentinite

CDR calderite FGL ferroglaucophane JMS jamesonite MRL marialite PRR pararealgar SP sphalerite VND vanadinite

CEL celadonite FHB ferrohornblende JOS joseite MRS miersite PRS proustite SPC sopcheite VRM vermiculite

CEN clinoenstatite FHQ ferroholmquistite JRD jordanite MRW merwinite PRV perovskite SPD spodumene VRN vernaditeCER cerussite FKR ferrokaersutite JUN junoite MS muscovite PSB pseudobrookite SPH sodium phlogopite VRS variscite

r r

r

rr

r

///////////

/////

/////////

/////////

KL-6

79m

KL06_30

325m

KL06_31

426m

KL93-4

120m

KL93-6

80m

NK

-94-2

1

125m

NK

-94-2

4

64m

IIP

CASE

XSH

IIO XSH IIO

XSH YIAT

XSH

XSH

VIAP

XSH

VIA

XSH

AQE

XSH

XSH

III XSH

XSH XSH

CASE

XSH

VIOP

XSH

VIO VIB

XSH

III XSH

IIO

VIO

XSH

VIO

XSH

III

IIO

IIP

VIO

OVER

VIA

VIA

VIA

VIA

VIA

OVER

VIA

VIA

VIA

VIA

AQ

E

VIA

OVER

VIAP

VIAP

VFD

VIA

VIAP

VIA

VIA

VIA

VIA

VIA

VIA

VIA

VIA

IIO

VIA

VIA

VIA

IID

VIA

IFO

VIA

VIA

VIA

OVER

VIA

VIAP

VIAP

VIA

VIA

VIA

IIM

VIA

VFD

VIA

1800

1600

175 230

706

335

635

1006

2040

818

603

351

292

635

479

240

544

525

1272

165

1616

828

1205

588

269

1098

776

860

2441

1766

2045

3497

2642

2134

379

2307

2007

1224

794

1498

746

2435

1399

846

1307

615

1823

728

1144

1925

1969

1731

4117

4115

5760

11290

4322

5506

4580

2691

1706

10630

37740

29890

2393

5574

6673

2847

2869

2809

1509

4680

3774

2665

2715

3936

3230

2572

1690

2079

2623

2254

5227

1883

852

51

1082

1461

2876

2235

707

1584

608

2262

1841

382

856

555

1863

1901

1326

2547

2644

2030

2981

1466

1905

1692

985

1309

2504

2650

722

64

741

1017

1071

2108

1084

2334

1340

1735

2529

679

1086

412

257

283

362

363

457

381

509

651

525

515

201

289

459

34

127

53

362

290

1506

1189

818

960

766

1175

639

681

536

672

703

582

449

502

862

1206

979

577

502

263

911

626

1224

2865

3305

453 899 329 884 1612 484 389 175 185

438 88 151 138 155 156 160 266 798 256

295 357 1534 58 46 217 151 463 330 141 412 248

496 125 543 143 734 418 179 419 711 2798 324 1977 1872 1787 1702 638 746 949 877 887 761 921 985 3103 5034 3675 2455 1788 932 926 1246 1679 1355 1347 747 811 247 924 883 433 1268 1022 614 1381 1395 1110 1021 669 492 776 501 241 194 314 198 204 267 297 578 327 170 149 172 235 263 814 296 80 199 1717 2103 268 366 786 1426 1318 954 361 111 224 554 1023 905 714 1155 1118 2018 669 423 481 367 3248 5854 15790 1171 1860 829 1010 750 456 621 827 364 175 1021 1108 1050 430 319 372 687 915 624 307 653 252 365 1927 2114 4282 1402 1069 42 34 31 29 29 1702 3475 2759 4729 3223 2710 1393 2384 1645 1636 1760 1472 1914 2741 584 47 29 31 35 33 57 32 254 1238 675 646 3610 795 1793 1137 1460 655 163 2057 1898 878 528 314 64 44

534

232

400

1961

3778

2606

1133

781

483

490

869

996

1565

1390

4134

1585

1615

2955

1787

2421

2437

4026

3000

2920

4462

2435

1827

1567

5268

7002

7991

4440

6956

3045

5508

1848

2583

5201

2942

1951

2762

2410

1765

2013

2036

752

1203

2327

1155

1331

2137

1380

2516

2044

240

270

680

100

520

340

450

530

440

370

250

990

290

670

390

750

450

750

700

1100

2352

3138

2822

1907

1500

1810

2167

1180

951

2005

1692

2465

3185

804

276

1346

442

386

1639

978

1811

614

903

1675

1251

2029

1984

1789

2169

1084

930

2159

1410

1556

1492

1686

2867

1666

1212

973

812

597

2414

3350

2204

2373

1504

1772

1049

1003

2512

3321

999

916

2008

707

1073

2135

282

1104

969

530

2379

636

1697

911

819

1438

801

2477

2532

761

594

3471

714

947

963

1259

572

830

732

1098

928

3360

858

1500

912

842

1137

660 320

50 140

317

38

48

97

103

171

86

60

49

94

66

54

52

32

90

29

62

27

49

27

22

41

43

37

88

63

69

103

85

76

17

94

105

71

50

81

57

88

70

45

79

56

152

54

107

207

272

182

1427

876

1003

2940

770

1388

2144

663

319

2037

11198

8101

324

1364

1444

285

649

424

123

429

315

128

317

211

125

135

60

66

102

272

268

70

54

33

79

103

235

263

119

264

116

253

365

103

142

137

315

356

163

1694

348

362

599

433

459

473

827

160

514

895

4719

3216

684

804

343

656

151

329

241

290

409

1066

10741

218

254

190

219

268

438

207

186

158

310

173

41

43

63

24

277

40

134

60

310

353

124

214

175

175

163

141

154

194

157

238

118

96

160

284

206

153

81

43

103

175

299

803

1724

56 113 89

135 174 47 45 34 58

20 24 20 20 28 18 23 29 36 23 46

32 96 23 13 15 8

18 81 21 36 21

38 12 52 21 66 31 26 27 54

200 23

182 235 157 172 79 70 59

101 124 69 71

100 972 746 579 504 330 203 367 132 278 269 151 788 291 49

257 166 148 633 203 110 274 341 374 414 331 102 184 105 73

176 145 413 512 698 154 480 57 67 52 44 61 97

236 226

2864 787 628 657 133 346 296 392 384 376 367 26 60

198 356 213 153 204 169 335 129 107 77

105 342 435 516 159 260 204 185 115 47 53 75 24 15 86

100 84 39 42 49 77

122 124 47

113 49 83

417 391 691 353 262 23 7 6 4 6

370 965 609

1308 858 889 372 643 340 430 525 339 523 780 182 818 52 7 9 5

13 13

105 483 234 233

1522 310 568 422

1408 4060 120

1147 793

1798 260 160 59 7

50

20

10

70

200

130

90

50

20

40

70

110

140

120

240

180

240

170

520

370

330

320

670

270

280

520

340

170

200

3

000

2

700

2

900

1

200

2

000

700

2

200

650

800

2

300

570

190

310

430

270

320

400

110

140

340

160

140

280

140

250

260

70

20

10

10

50

30

40

50

40

40

30

90

30

50

30

110

120

30

80

70

110

150

200

180

240

480

300

200

120

190

190

240

320

62

31

124

31

93

156

93

218

62

62

93

62

187

156

93

187

62

62

93

93

124

156

124

249

218

156

124

124

124

218

560

62

93

93

124

124

62

124

124

31

62

93

31

31

62

-31

62

62

31

156

31

93

62

62

156

93

342

404

93

93

498

62

93

93

156

62

93

62

93

62

187

62

156

156

93

156

1400mRL 1400mRL

1500mRL1500mRL

1600mRL 1600mRL

1700mRL1700mRL

1800mRL 1800mRL

-400m

-400m

-300m

-300m

-200m

-200m

-100m

-100m

0m

0m

100m

100m

200m

200m

300m

300m

400m

400m

Lithology Legend

Silica Alteration

Sulphide Alteration

Casing

IFO

..

.. IFP

Intermediate Intrusive

////

Intermediate Intrusive Porphyry

Mafic Intrusive

Sediment

Felsic Volcanic

Intermediate Volcanic

Chlorite-sericite-py Schist

Felsic-intermediate tuff

Fault Breccia

Quartz Vein

Au ppb on Left hand side of Drill Trace

Cu ppm on Right hand side of Drill Trace

Scale

1:1000

DATE

23/04/2007

REF No.

1

SHEET

1 of 1

FILE

Kliyul_section_Au_Cu_LITH

100m0 50

Kliyul Project

2006 Drilling

Section bearing 220 Degrees

Cu ppm and Au ppb

Geoinformatics Exploration

31

Appendix 4: Statement of costs (Expenditures and Assessment Data)

Takla - Redton, Kliyul and Mesilinka Projects 2006 Assessment Report Statement of Costs

2006 BC Projects Expenditures (Dec/ 2005 - Nov/2006) Total Usable for Redton Kliyul Mesilinka TotalRedton Kliyul Mesilinka Blackjack Blackwater Expend. Assess. Assess. Assess. Assess. Assess.

Office Charges (Perth & Vanc)Administration (Vancouver) 42,852 6,300 6,000 55,152 - Office costs (Vancouver) 306 170 110 586 - Perth geoscience 429,077 61,226 158,469 1,187 678 650,637 648,773 429,077 61,226 158,469 648,773 Perth travel expenses 18,596 1,684 14,342 34,622 - - - - - - -

Total 490,831 69,381 178,921 1,187 678 740,998 648,773 429,077 61,226 158,469 648,773

Field Costs - DirectAdministration labour 31,441 700 32,141 32,141 22,499 4,821 4,821 32,141 Geology labour 65,388 2,042 67,430 67,430 47,201 10,114 10,114 67,430 Geochemistry labour 80,861 4,100 84,961 84,961 59,473 12,744 12,744 84,961 Geophysics labour 840 696 1,536 1,536 1,536 1,536 Data acquisition 7,244 1,450 5,088 13,782 13,782 7,244 1,450 5,088 13,782 Diamond Drilling (contractor charges) 602,253 95,329 697,582 697,582 544,114 153,468 697,582 Drilling supplies 54,214 54,214 54,214 42,287 11,927 54,214 Equipment & supplies (field) 21,052 451 21,504 21,504 17,203 2,150 2,150 21,504 Field rentals 3,883 3,883 3,883 3,262 621 3,883 Assays (core) 46,462 46,462 46,462 39,028 7,434 46,462 Assays (rock, soil, silt) 34,490 3,415 37,905 37,905 23,501 1,516 12,888 37,905 First aid & Safety 4,361 466 4,827 4,827 3,861 483 483 4,827 - - -

Total 952,489 101,134 12,603 - - 1,066,226 1,066,226 811,208 206,729 48,288 1,066,226

Field Costs - CampCamp construction (labour) 62,454 236 62,690 62,690 50,152 6,269 6,269 62,690 Camp maintence (labour) 23,218 23,218 23,218 18,574 2,322 2,322 23,218 Cooking (labour) 116,141 116,141 116,141 92,913 11,614 11,614 116,141 Accommodation 7,494 7,494 7,494 5,995 749 749 7,494 Food 57,668 1,120 58,787 58,787 47,030 5,879 5,879 58,787 Camp equipment 94,191 20,988 115,179 115,179 80,625 23,036 11,518 115,179 Camp supplies 34,837 34,837 34,837 27,870 3,484 3,484 34,837 Camp fuel 13,926 13,926 13,926 11,141 1,393 1,393 13,926 Camp rentals 39,563 39,563 39,563 31,651 3,956 3,956 39,563 Communications 18,488 18,488 18,488 14,790 1,849 1,849 18,488 Expedting 44,729 44,729 44,729 35,784 4,473 4,473 44,729 - - - -

- - Total 512,709 22,343 - - - 535,052 535,052 416,524 65,023 53,505 535,052

Field Costs - TransportTravel time (wages) 425 700 1,125 1,125 900 113 113 1,125 Air fares 28,843 28,843 28,843 23,074 2,884 2,884 28,843 Travel accommodation & meals 17,701 8 17,710 17,710 14,168 1,771 1,771 17,710 Helicopter charter 312,553 84,680 60,059 457,292 457,292 312,553 84,680 60,059 457,292 Fixed Wing charter 27,128 27,128 27,128 21,702 2,713 2,713 27,128 Ground transport 44,712 44,712 44,712 31,299 8,942 4,471 44,712 Equipment & supplies 1,214 1,214 1,214 971 121 121 1,214 Freight 25,856 2,287 28,143 28,143 19,700 5,629 2,814 28,143 Expediting 150,794 150,794 150,794 105,555 30,159 15,079 150,794

- - - Total 609,226 86,967 60,767 - - 756,960 756,960 529,922 137,012 90,025 756,960

Field MiscellaneousLand acquisition, maintenance (labour) 2,100 2,592 9,100 13,792 Staking fees 7,583 3,240 41,517 1,983 54,323 Permitting, environmental & reclamation 3,051 700 1,484 5,235 Aboriginal affairs - Miscellaneous 60 60

Total 12,794 6,532 52,101 - 1,983 73,410 - # - - -

MiscellaneousLegal fees - Assessment fees 45,503 45,503 Option payments 100,000 100,000 Accounting, bank fees 8,343 8,343 -

Total 153,846 - - - - 153,846 - - - -

Project Total 2,731,895 286,356 304,392 1,187 2,662 3,326,492 3,007,010 2,186,731 469,991 350,289 3,007,011

14/05/2007

Takla Redton Project - 2006 Labour (days)Person Affiliation May Jun Jul Aug Sep Oct Total

Tonny Worth Geoinformatics 17 15 31 24 6 93John Mair Geoinformatics 3 31 25 25 4 88Tom Marshall Geoinformatics 17 31 19 25 4 96McLean Trott Geoinformatics 17 31 19 23 90Darryn Hitchcock Geoinformatics 17 25 30 24 2 98Gemma Cryan Geoinformatics 11 28 31 25 2 97Robin McQuinn Geoinformatics 27 25 30 2 84Rod Kirkham Geoinformatics 15 15Nick Archibald Geoinformatics 3 3 6Gerry Bidwell Geoinformatics 5 3 3 11Rob Stuart Geoinformatics 6 6Mark Stewart Geoinformatics 3 3Jennifer MacLaughlan Geoinformatics 7 7Steve Garwin Geoinformatics 7 7

Paul MacDonald Minconsult Mineral Expl 3 30 10 31 24 6 104Chris Wolverton Minconsult Mineral Expl 3 30 23 22 29 5 112Tim Pynn Minconsult Mineral Expl 3 30 31 64Adrian Minconsult Mineral Expl 3 20 23

Minconsult Mineral Expl 3 13 16Erica Austin Minconsult Mineral Expl 15 24 30 69Bart Sam Minconsult Mineral Expl 5 31 13 28 5 82Henry Prince Minconsult Mineral Expl 5 10 15Richard Greenwood Minconsult Mineral Expl 6 6Derek Monk Minconsult Mineral Expl 20 20Kevin Bazil Minconsult Mineral Expl 26 6 32Bernard Haskell Minconsult Mineral Expl 14 28 8 50Richard MacDonald Minconsult Mineral Expl 6 21 6 33Aaron Clarke Minconsult Mineral Expl 6 6Steve Toki Minconsult Mineral Expl 22 22

Will Elliot Nugget Expediting 17 31 12 30 4 94Camille Elliot Nugget Expediting 15 31 12 30 2 90Sandy Nugget Expediting 30 6 36

Dan Hill Full Force Drilling 3 3Josh Hill Full Force Drilling 3 31 18 30 2 84Miles Jecowsky Full Force Drilling 31 18 30 2 81Jessie Maxon Full Force Drilling 3 31 18 30 2 84Tom Hill Full Force Drilling 3 31 18 30 2 84

helicopter pilot Interior Helicopters 3 30 31 31 30 3 128

Total 18 342 590 467 557 65 2039

Of the 2039 total mandays worked out of the Redton camp the project distribution is Redton 1668 daysKliyul 209 days

Mesilinka 162 daysTotal 2039 days

Kliyul - Mesilinka Assessment 2006 Work (applied Feb/07)

Property Block Date No. of Claims Event No. Work Amount UsedAssessment

Required PAC FeesKliyul Block 1 16-Feb-07 40 4133112 100,000.00 46,938.87 53,061.13 4,706.74 Kliyul Block 1a 21-Feb-07 47 4133956 60,000.00 4,580.87 55,419.13 229.67 Kliyul Block 2 15-Feb-07 62 4132905 150,000.00 70,042.37 79,957.63 6,995.06 Kliyul Block 3 16-Feb-07 51 4133031 150,000.00 56,450.65 93,549.35 5,647.80

Total 460,000.00 178,012.76 281,987.24 17,579.27

Mesilinka Block 4 16-Feb-07 60 4133170 80,000.00 73,754.26 6,245.74 7,393.53 Mesilinka Block 5 20-Feb-07 37 4133736 80,000.00 33,638.34 46,361.66 3,372.25 Mesilinka Block 6 20-Feb-07 4 4133739 8,000.00 5,011.87 2,988.13 502.56 Mesilinka Block 7 20-Feb-07 48 4133750 62,000.00 60,176.70 1,823.30 6,034.16 Mesilinka Block 8 20-Feb-07 16 4133742 9,000.00 8,507.55 492.45 853.09 Mesilinka Block 9 20-Feb-07 9 4133748 5,000.00 4,798.99 201.01 481.21 Mesilinka Block 10 26-Feb-07 8 4134630 3,000.00 2,016.31 983.69 202.05

Total 247,000.00 187,904.02 59,095.98 18,838.85

Kliyul-Mesilinka Total 707,000.00 365,916.78 341,083.22 36,418.12

kliyul - mesilinka assessment 2006 work (applied feb/07)

Documents